Influence of intra-event-based flood regime on sediment flow behavior from a typical agro-catchment of the Chinese Loess Plateau

[Display omitted] •Intra event-based flood regimes were analyzed at catchment scale.•Sediment flow behavior under different flood regimes was discussed.•Sediment reduction caused by runoff self-regulation should not be neglected. The pluvial erosion process is significantly affected by tempo-spatial...

Celý popis

Uložené v:

Podrobná bibliografia
Vydané v:	Journal of hydrology (Amsterdam) Ročník 538; s. 71 - 81
Hlavní autori:	Zhang, Le-Tao, Li, Zhan-Bin, Wang, He, Xiao, Jun-Bo
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Elsevier B.V 01.07.2016
Predmet:	agricultural watersheds analysis of variance Catchments China discriminant analysis Dynamics energy equations Exports Flood regime Floods Freshwater Hierarchical clustering approach Internal sediment reduction International trade loess Mathematical analysis Runoff Runoff self-regulation mechanism Sediment flow behavior sediment transport sediment yield Sediments soil soil erosion suspended sediment China, People's Rep., Loess Plateau China Flood regime Sediment flow behavior Internal sediment reduction Runoff self-regulation mechanism Hierarchical clustering approach
ISSN:	0022-1694, 1879-2707
On-line prístup:	Získať plný text
Tagy:	Pridať tag Žiadne tagy, Buďte prvý, kto otaguje tento záznam!

Abstract	[Display omitted] •Intra event-based flood regimes were analyzed at catchment scale.•Sediment flow behavior under different flood regimes was discussed.•Sediment reduction caused by runoff self-regulation should not be neglected. The pluvial erosion process is significantly affected by tempo-spatial patterns of flood flows. However, despite their importance, only a few studies have investigated the sediment flow behavior that is driven by different flood regimes. The study aims to investigate the effect of intra-event-based flood regimes on the dynamics of sediment exports at Tuanshangou catchment, a typical agricultural catchment (unmanaged) in the hilly loess region on the Chinese Loess Plateau. Measurements of 193 flood events and 158 sediment-producing events were collected from Tuanshangou station between 1961 and 1969. The combined methods of hierarchical clustering approach, discriminant analysis and One-Way ANOVA were used to classify the flood events in terms of their event-based flood characteristics, including flood duration, peak discharge, and event flood runoff depth. The 193 flood events were classified into five regimes, and the mean statistical features of each regime significantly differed. Regime A includes flood events with the shortest duration (76min), minimum flood crest (0.045ms−1), least runoff depth (0.2mm), and highest frequency. Regime B includes flood events with a medium duration (274min), medium flood crest (0.206ms−1), and minor runoff depth (0.7mm). Regime C includes flood events with the longest duration (822min), medium flood crest (0.236ms−1), and medium runoff depth (1.7mm). Regime D includes flood events with a medium duration (239min), large flood crest (4.21ms−1), and large runoff depth (10mm). Regime E includes flood events with a medium duration (304min), maximum flood crest (8.62ms−1), and largest runoff depth (25.9mm). The sediment yield by different flood regimes is ranked as follows: Regime E>Regime D>Regime B>Regime C>Regime A. In terms of event-based average and maximum suspended sediment concentration, these regimes are ordered as follows: Regime E>Regime D>Regime C>Regime B>Regime A. Regimes D and E produce the most runoff volume and the largest amount of sediments, which indicates that these regimes must be at the focus of runoff regulation to control the sediments. Given that the event flood runoff depth remains constant, the sediment yield by different flood regimes is regulated to varying degrees by altering the event-based runoff–sediment relationship. Compared with Regime A, the average decrease rates in the area-specific sediment yield for Regimes B, C, and D are 33%, 78%, and 62%, respectively. The regulative effect of the flood regime conversion on sediment export can be described with several variables that indicate the depth-specific characteristics of individual flood events. Flood regimes indicate the runoff erosivity dynamics and the runoff energy dissipation rates in eroding soil and delivering sediments. Therefore, the flood-regime-dependent sediment flow behavior differs across all regimes. Overall, the predominated controlling factors that influence the final sediment export are regime based. Empirical regime-based runoff–sediment relationships were established via multiple stepwise regressions. The suspended sediment concentration that is driven by different flood regimes can be described by the power function or logarithmic–linear function of runoff-related variables, including instantaneous discharge, runoff erosive power, and event-based flow variability. The regressive equations can explain the major driving forces behind the suspended sediment concentration dynamics. This study highlights the potentials of runoff self-regulation in controlling soil erosion and sediment delivery. The results may provide some evidence for flood regime classification, improve the overall evaluation of the sediment reduction benefits of the runoff regulation system, enrich runoff regulation theory, and improve the runoff control at the catchment scale.
AbstractList	The pluvial erosion process is significantly affected by tempo-spatial patterns of flood flows. However, despite their importance, only a few studies have investigated the sediment flow behavior that is driven by different flood regimes. The study aims to investigate the effect of intra-event-based flood regimes on the dynamics of sediment exports at Tuanshangou catchment, a typical agricultural catchment (unmanaged) in the hilly loess region on the Chinese Loess Plateau. Measurements of 193 flood events and 158 sediment-producing events were collected from Tuanshangou station between 1961 and 1969. The combined methods of hierarchical clustering approach, discriminant analysis and One-Way ANOVA were used to classify the flood events in terms of their event-based flood characteristics, including flood duration, peak discharge, and event flood runoff depth. The 193 flood events were classified into five regimes, and the mean statistical features of each regime significantly differed. Regime A includes flood events with the shortest duration (76min), minimum flood crest (0.045ms-1), least runoff depth (0.2mm), and highest frequency. Regime B includes flood events with a medium duration (274min), medium flood crest (0.206ms-1), and minor runoff depth (0.7mm). Regime C includes flood events with the longest duration (822min), medium flood crest (0.236ms-1), and medium runoff depth (1.7mm). Regime D includes flood events with a medium duration (239min), large flood crest (4.21ms-1), and large runoff depth (10mm). Regime E includes flood events with a medium duration (304min), maximum flood crest (8.62ms-1), and largest runoff depth (25.9mm). The sediment yield by different flood regimes is ranked as follows: Regime E>Regime D>Regime B>Regime C>Regime A. In terms of event-based average and maximum suspended sediment concentration, these regimes are ordered as follows: Regime E>Regime D>Regime C>Regime B>Regime A. Regimes D and E produce the most runoff volume and the largest amount of sediments, which indicates that these regimes must be at the focus of runoff regulation to control the sediments. Given that the event flood runoff depth remains constant, the sediment yield by different flood regimes is regulated to varying degrees by altering the event-based runoff-sediment relationship. Compared with Regime A, the average decrease rates in the area-specific sediment yield for Regimes B, C, and D are 33%, 78%, and 62%, respectively. The regulative effect of the flood regime conversion on sediment export can be described with several variables that indicate the depth-specific characteristics of individual flood events. Flood regimes indicate the runoff erosivity dynamics and the runoff energy dissipation rates in eroding soil and delivering sediments. Therefore, the flood-regime-dependent sediment flow behavior differs across all regimes. Overall, the predominated controlling factors that influence the final sediment export are regime based. Empirical regime-based runoff-sediment relationships were established via multiple stepwise regressions. The suspended sediment concentration that is driven by different flood regimes can be described by the power function or logarithmic-linear function of runoff-related variables, including instantaneous discharge, runoff erosive power, and event-based flow variability. The regressive equations can explain the major driving forces behind the suspended sediment concentration dynamics. This study highlights the potentials of runoff self-regulation in controlling soil erosion and sediment delivery. The results may provide some evidence for flood regime classification, improve the overall evaluation of the sediment reduction benefits of the runoff regulation system, enrich runoff regulation theory, and improve the runoff control at the catchment scale. [Display omitted] •Intra event-based flood regimes were analyzed at catchment scale.•Sediment flow behavior under different flood regimes was discussed.•Sediment reduction caused by runoff self-regulation should not be neglected. The pluvial erosion process is significantly affected by tempo-spatial patterns of flood flows. However, despite their importance, only a few studies have investigated the sediment flow behavior that is driven by different flood regimes. The study aims to investigate the effect of intra-event-based flood regimes on the dynamics of sediment exports at Tuanshangou catchment, a typical agricultural catchment (unmanaged) in the hilly loess region on the Chinese Loess Plateau. Measurements of 193 flood events and 158 sediment-producing events were collected from Tuanshangou station between 1961 and 1969. The combined methods of hierarchical clustering approach, discriminant analysis and One-Way ANOVA were used to classify the flood events in terms of their event-based flood characteristics, including flood duration, peak discharge, and event flood runoff depth. The 193 flood events were classified into five regimes, and the mean statistical features of each regime significantly differed. Regime A includes flood events with the shortest duration (76min), minimum flood crest (0.045ms−1), least runoff depth (0.2mm), and highest frequency. Regime B includes flood events with a medium duration (274min), medium flood crest (0.206ms−1), and minor runoff depth (0.7mm). Regime C includes flood events with the longest duration (822min), medium flood crest (0.236ms−1), and medium runoff depth (1.7mm). Regime D includes flood events with a medium duration (239min), large flood crest (4.21ms−1), and large runoff depth (10mm). Regime E includes flood events with a medium duration (304min), maximum flood crest (8.62ms−1), and largest runoff depth (25.9mm). The sediment yield by different flood regimes is ranked as follows: Regime E>Regime D>Regime B>Regime C>Regime A. In terms of event-based average and maximum suspended sediment concentration, these regimes are ordered as follows: Regime E>Regime D>Regime C>Regime B>Regime A. Regimes D and E produce the most runoff volume and the largest amount of sediments, which indicates that these regimes must be at the focus of runoff regulation to control the sediments. Given that the event flood runoff depth remains constant, the sediment yield by different flood regimes is regulated to varying degrees by altering the event-based runoff–sediment relationship. Compared with Regime A, the average decrease rates in the area-specific sediment yield for Regimes B, C, and D are 33%, 78%, and 62%, respectively. The regulative effect of the flood regime conversion on sediment export can be described with several variables that indicate the depth-specific characteristics of individual flood events. Flood regimes indicate the runoff erosivity dynamics and the runoff energy dissipation rates in eroding soil and delivering sediments. Therefore, the flood-regime-dependent sediment flow behavior differs across all regimes. Overall, the predominated controlling factors that influence the final sediment export are regime based. Empirical regime-based runoff–sediment relationships were established via multiple stepwise regressions. The suspended sediment concentration that is driven by different flood regimes can be described by the power function or logarithmic–linear function of runoff-related variables, including instantaneous discharge, runoff erosive power, and event-based flow variability. The regressive equations can explain the major driving forces behind the suspended sediment concentration dynamics. This study highlights the potentials of runoff self-regulation in controlling soil erosion and sediment delivery. The results may provide some evidence for flood regime classification, improve the overall evaluation of the sediment reduction benefits of the runoff regulation system, enrich runoff regulation theory, and improve the runoff control at the catchment scale. The pluvial erosion process is significantly affected by tempo-spatial patterns of flood flows. However, despite their importance, only a few studies have investigated the sediment flow behavior that is driven by different flood regimes. The study aims to investigate the effect of intra-event-based flood regimes on the dynamics of sediment exports at Tuanshangou catchment, a typical agricultural catchment (unmanaged) in the hilly loess region on the Chinese Loess Plateau. Measurements of 193 flood events and 158 sediment-producing events were collected from Tuanshangou station between 1961 and 1969. The combined methods of hierarchical clustering approach, discriminant analysis and One-Way ANOVA were used to classify the flood events in terms of their event-based flood characteristics, including flood duration, peak discharge, and event flood runoff depth. The 193 flood events were classified into five regimes, and the mean statistical features of each regime significantly differed. Regime A includes flood events with the shortest duration (76min), minimum flood crest (0.045ms−1), least runoff depth (0.2mm), and highest frequency. Regime B includes flood events with a medium duration (274min), medium flood crest (0.206ms−1), and minor runoff depth (0.7mm). Regime C includes flood events with the longest duration (822min), medium flood crest (0.236ms−1), and medium runoff depth (1.7mm). Regime D includes flood events with a medium duration (239min), large flood crest (4.21ms−1), and large runoff depth (10mm). Regime E includes flood events with a medium duration (304min), maximum flood crest (8.62ms−1), and largest runoff depth (25.9mm). The sediment yield by different flood regimes is ranked as follows: Regime E>Regime D>Regime B>Regime C>Regime A. In terms of event-based average and maximum suspended sediment concentration, these regimes are ordered as follows: Regime E>Regime D>Regime C>Regime B>Regime A. Regimes D and E produce the most runoff volume and the largest amount of sediments, which indicates that these regimes must be at the focus of runoff regulation to control the sediments. Given that the event flood runoff depth remains constant, the sediment yield by different flood regimes is regulated to varying degrees by altering the event-based runoff–sediment relationship. Compared with Regime A, the average decrease rates in the area-specific sediment yield for Regimes B, C, and D are 33%, 78%, and 62%, respectively. The regulative effect of the flood regime conversion on sediment export can be described with several variables that indicate the depth-specific characteristics of individual flood events. Flood regimes indicate the runoff erosivity dynamics and the runoff energy dissipation rates in eroding soil and delivering sediments. Therefore, the flood-regime-dependent sediment flow behavior differs across all regimes. Overall, the predominated controlling factors that influence the final sediment export are regime based. Empirical regime-based runoff–sediment relationships were established via multiple stepwise regressions. The suspended sediment concentration that is driven by different flood regimes can be described by the power function or logarithmic–linear function of runoff-related variables, including instantaneous discharge, runoff erosive power, and event-based flow variability. The regressive equations can explain the major driving forces behind the suspended sediment concentration dynamics. This study highlights the potentials of runoff self-regulation in controlling soil erosion and sediment delivery. The results may provide some evidence for flood regime classification, improve the overall evaluation of the sediment reduction benefits of the runoff regulation system, enrich runoff regulation theory, and improve the runoff control at the catchment scale.
Author	Xiao, Jun-Bo Wang, He Zhang, Le-Tao Li, Zhan-Bin
Author_xml	– sequence: 1 givenname: Le-Tao surname: Zhang fullname: Zhang, Le-Tao organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, PR China – sequence: 2 givenname: Zhan-Bin surname: Li fullname: Li, Zhan-Bin email: zbli@ms.iswc.ac.cn organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, PR China – sequence: 3 givenname: He surname: Wang fullname: Wang, He organization: Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi Province 712100, PR China – sequence: 4 givenname: Jun-Bo surname: Xiao fullname: Xiao, Jun-Bo organization: Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi Province 712100, PR China
BookMark	eNqNkb1u2zAUhYkgBeqkfYQCHLtI5Y_-iAxFYbRpAAPp0M7EFXUV0ZBJl6RdeOujh4ozZUm4kJf8zhn4XZFL5x0S8omzkjPefNmW2-k0BD-XIo8l4yVr-AVZ8a5VhWhZe0lWjAlR8EZV78lVjFuWl5TVivy_c-N8QGeQ-pFalwIUeESXih4iDnScvR9owAe7y4Sj-S6fXFoe_tEeJzhaH-gY_I4CTae9NTBTeAi-MJDM9MTm5jQhXU_WYUS68Rgj_TVDQjh8IO9GmCN-fN6vyZ8f33-vfxab-9u79bdNAZXkqahr1cuuqUSHMEiQWDOBwGDsetPUCgY-AmsVU62qjaiV7Nq-aZG34wBcKJDX5PO5dx_83wPGpHc2GpxncOgPUfNO1FUrpKjehopGMv4GlHWNUuwJrc-oCT7GgKPeB7uDcNKc6cWj3upnj3rxqBnX2WPO3bzIGZsgWb-4svOr6a_nNOa_PVoMOhq76B5sQJP04O0rDY_Vd7-2
CitedBy_id	crossref_primary_10_1016_j_heliyon_2024_e39153 crossref_primary_10_1016_j_jhydrol_2019_124422 crossref_primary_10_1016_j_jhydrol_2023_129433 crossref_primary_10_1002_ldr_2645 crossref_primary_10_1016_j_catena_2023_107292 crossref_primary_10_2489_jswc_2020_00012 crossref_primary_10_1016_j_scitotenv_2019_01_378 crossref_primary_10_2166_nh_2017_003 crossref_primary_10_1016_j_jhydrol_2019_04_040 crossref_primary_10_3390_su141811573 crossref_primary_10_3390_w12051319 crossref_primary_10_1029_2019WR025840 crossref_primary_10_1016_j_catena_2025_109155 crossref_primary_10_2134_jeq2018_06_0229 crossref_primary_10_1016_j_scitotenv_2020_137935 crossref_primary_10_1016_j_scitotenv_2023_166032 crossref_primary_10_1016_j_jhydrol_2024_131407 crossref_primary_10_1016_j_scs_2020_102044 crossref_primary_10_3390_su152115642 crossref_primary_10_1016_j_envsoft_2019_05_007 crossref_primary_10_1002_esp_5123 crossref_primary_10_1002_hyp_15092 crossref_primary_10_3390_w14060913 crossref_primary_10_1016_j_ecolind_2024_111690 crossref_primary_10_1016_j_ejrh_2025_102654 crossref_primary_10_1002_ldr_5441 crossref_primary_10_1016_j_scitotenv_2018_07_248 crossref_primary_10_1002_hyp_13782 crossref_primary_10_1016_j_catena_2022_106451 crossref_primary_10_1038_s41598_021_95111_6 crossref_primary_10_1007_s11676_024_01759_x crossref_primary_10_1016_j_catena_2019_104376 crossref_primary_10_1016_j_jhydrol_2025_132694 crossref_primary_10_1007_s11707_018_0732_x crossref_primary_10_1016_j_heliyon_2024_e30550 crossref_primary_10_1016_j_jhydrol_2018_02_084 crossref_primary_10_1016_j_catena_2021_105864 crossref_primary_10_3390_w11040834 crossref_primary_10_1016_j_ecoleng_2017_09_005
Cites_doi	10.1002/esp.2176 10.13031/2013.30724 10.1016/0022-1694(95)02704-S 10.1007/s00267-008-9122-6 10.1016/j.still.2009.04.002 10.1002/hyp.10309 10.1007/s00254-006-0513-9 10.1016/j.jhydrol.2015.06.046 10.1002/hyp.6391 10.1002/hyp.10576 10.1016/j.geoderma.2009.07.003 10.1016/j.jhydrol.2011.12.035 10.2136/sssaj2000.6451759x 10.1016/j.jhydrol.2014.04.014 10.5402/2012/310927 10.1002/esp.1649 10.1016/j.jhydrol.2011.09.043 10.1016/j.catena.2010.04.005 10.1177/0309133309341426 10.1371/journal.pone.0117989 10.1016/j.gloplacha.2011.11.008 10.1016/j.jhydrol.2010.07.019 10.1016/j.catena.2006.03.002 10.1029/1999WR900340 10.1061/(ASCE)HE.1943-5584.0001117 10.1016/j.agee.2004.01.032 10.1016/j.jhydrol.2010.11.039 10.1016/S0341-8162(01)00161-8 10.1016/j.jhydrol.2013.04.028 10.1007/BF02837377 10.1097/SS.0000000000000068 10.1016/S1001-6279(09)60009-3 10.1016/j.catena.2011.11.001 10.1016/j.jhydrol.2015.04.058 10.1016/j.jaridenv.2005.03.030 10.1016/j.jhydrol.2014.04.032 10.1016/S0341-8162(99)00059-4 10.1007/s11069-015-1996-z 10.1016/j.jhydrol.2006.11.016 10.1016/j.catena.2012.05.013 10.1016/j.catena.2012.07.004 10.1016/j.jhydrol.2012.09.019 10.1016/j.jhydrol.2015.01.045 10.1002/hyp.8317 10.1016/j.catena.2013.03.017 10.1016/S0341-8162(99)00009-0 10.1007/s11269-008-9361-6 10.1097/01.ss.0000117784.98510.46 10.1016/j.geomorph.2007.03.001 10.1016/j.advwatres.2005.07.014
ContentType	Journal Article
Copyright	2016
Copyright_xml	– notice: 2016
DBID	AAYXX CITATION 7QH 7ST 7TG 7UA C1K F1W H96 KL. L.G SOI 7S9 L.6 8FD FR3 KR7
DOI	10.1016/j.jhydrol.2016.01.061
DatabaseName	CrossRef Aqualine Environment Abstracts Meteorological & Geoastrophysical Abstracts Water Resources Abstracts Environmental Sciences and Pollution Management ASFA: Aquatic Sciences and Fisheries Abstracts Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources Meteorological & Geoastrophysical Abstracts - Academic Aquatic Science & Fisheries Abstracts (ASFA) Professional Environment Abstracts AGRICOLA AGRICOLA - Academic Technology Research Database Engineering Research Database Civil Engineering Abstracts
DatabaseTitle	CrossRef Aquatic Science & Fisheries Abstracts (ASFA) Professional Meteorological & Geoastrophysical Abstracts Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources ASFA: Aquatic Sciences and Fisheries Abstracts Aqualine Environment Abstracts Meteorological & Geoastrophysical Abstracts - Academic Water Resources Abstracts Environmental Sciences and Pollution Management AGRICOLA AGRICOLA - Academic Technology Research Database Civil Engineering Abstracts Engineering Research Database
DatabaseTitleList	Technology Research Database Aquatic Science & Fisheries Abstracts (ASFA) Professional AGRICOLA
DeliveryMethod	fulltext_linktorsrc
Discipline	Geography
EISSN	1879-2707
EndPage	81
ExternalDocumentID	10_1016_j_jhydrol_2016_01_061 S0022169416300014
GeographicLocations	China, People's Rep., Loess Plateau China
GeographicLocations_xml	– name: China, People's Rep., Loess Plateau – name: China
GroupedDBID	--K --M -~X .~1 0R~ 1B1 1RT 1~. 1~5 29K 4.4 457 4G. 5GY 5VS 6TJ 7-5 71M 8P~ 9JM 9JN AABNK AABVA AACTN AAEDT AAEDW AAIAV AAIKJ AAKOC AALCJ AALRI AAOAW AAQFI AAQXK AATLK AAXUO ABEFU ABFNM ABGRD ABJNI ABMAC ABQEM ABQYD ABTAH ABXDB ABYKQ ACDAQ ACGFS ACIUM ACLVX ACNCT ACRLP ACSBN ADBBV ADEZE ADMUD ADQTV AEBSH AEKER AENEX AEQOU AFFNX AFKWA AFTJW AFXIZ AGHFR AGUBO AGYEJ AHHHB AIEXJ AIKHN AITUG AJBFU AJOXV ALMA_UNASSIGNED_HOLDINGS AMFUW AMRAJ ASPBG ATOGT AVWKF AXJTR AZFZN BKOJK BLXMC CBWCG CS3 D-I DU5 EBS EFJIC EFLBG EJD EO8 EO9 EP2 EP3 FA8 FDB FEDTE FGOYB FIRID FNPLU FYGXN G-2 G-Q GBLVA HLV HMA HVGLF HZ~ H~9 IHE IMUCA J1W K-O KOM LW9 LY3 M41 MO0 N9A O-L O9- OAUVE OZT P-8 P-9 P2P PC. Q38 R2- RIG ROL RPZ SAB SCC SDF SDG SDP SEP SES SEW SPC SPCBC SPD SSA SSE SSZ T5K TN5 UQL VOH WUQ Y6R ZCA ZMT ZY4 ~02 ~G- ~KM 9DU AAHBH AATTM AAXKI AAYWO AAYXX ABUFD ABWVN ACLOT ACRPL ACVFH ADCNI ADNMO ADVLN AEIPS AEUPX AFJKZ AFPUW AGQPQ AIGII AIIUN AKBMS AKRWK AKYEP ANKPU APXCP CITATION EFKBS ~HD 7QH 7ST 7TG 7UA C1K F1W H96 KL. L.G SOI 7S9 L.6 8FD FR3 KR7
ID	FETCH-LOGICAL-a431t-559b386428ead3a3e502ea0af8bc659ad1fa07909795c259387b67e17fda129a3
ISICitedReferencesCount	41
ISICitedReferencesURI	http://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=Summon&SrcAuth=ProQuest&DestLinkType=CitingArticles&DestApp=WOS_CPL&KeyUT=000378360600007&url=https%3A%2F%2Fcvtisr.summon.serialssolutions.com%2F%23%21%2Fsearch%3Fho%3Df%26include.ft.matches%3Dt%26l%3Dnull%26q%3D
ISSN	0022-1694
IngestDate	Wed Oct 01 14:53:21 EDT 2025 Sat Sep 27 21:56:51 EDT 2025 Tue Oct 07 09:58:10 EDT 2025 Sat Nov 29 04:33:38 EST 2025 Tue Nov 18 22:42:24 EST 2025 Fri Feb 23 02:26:58 EST 2024
IsPeerReviewed	true
IsScholarly	true
Keywords	Flood regime Sediment flow behavior Internal sediment reduction Runoff self-regulation mechanism Hierarchical clustering approach
Language	English
LinkModel	OpenURL
MergedId	FETCHMERGED-LOGICAL-a431t-559b386428ead3a3e502ea0af8bc659ad1fa07909795c259387b67e17fda129a3
Notes	ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23
PQID	1808699001
PQPubID	23462
PageCount	11
ParticipantIDs	proquest_miscellaneous_1825472324 proquest_miscellaneous_1825426301 proquest_miscellaneous_1808699001 crossref_primary_10_1016_j_jhydrol_2016_01_061 crossref_citationtrail_10_1016_j_jhydrol_2016_01_061 elsevier_sciencedirect_doi_10_1016_j_jhydrol_2016_01_061
PublicationCentury	2000
PublicationDate	July 2016 2016-07-00 20160701
PublicationDateYYYYMMDD	2016-07-01
PublicationDate_xml	– month: 07 year: 2016 text: July 2016
PublicationDecade	2010
PublicationTitle	Journal of hydrology (Amsterdam)
PublicationYear	2016
Publisher	Elsevier B.V
Publisher_xml	– name: Elsevier B.V
References	Xu (b0255) 1999; 36 Emmanuel, Andrieu, Leblois, Janey, Payrastre (b0040) 2015; 531 Gao, Fu, Zhang, Zhang, Wan (b0095) 2013; 29 Zhang, Li, Wang (b0280) 2015; 31 Zheng, Chen (b0295) 2015; 10 Zhou (b0325) 1997; 4 Cai, Liu, Liu (b0015) 2004; 23 Hancock (b0110) 2009; 152 Cammeraat (b0020) 2004; 104 Gao, Jiang, Wei, Mu, Wang, Zhao, Sun (b0090) 2015; 29 Wei, Chen, Fu, Huang, Wu, Gui (b0240) 2007; 335 Morin, Goodrich, Maddox, Gao, Gupta, Sorooshian (b0165) 2006; 29 Ministry of Water Conservancy and Electric Power, PRC, 1975. Tentative specification of hydrometry (in Chinese). Fang, Cai, Chen, Li (b0055) 2008; 42 Fang, Shi, Li, Guo, Liu, Ai (b0070) 2012; 99 Williams, J.R., 1975. Sediment-yield prediction with universal equation using runoff energy factor. In: Present and Pro-spective Technology for Predicting Sediment Yield and Sources. Proceedings of the Sediment-yield Workshop, USDA Sedimentation Lab., Oxford, MS, November 28–30, 1972. ARS-S-40, pp. 244–252. Strauch, MacKenzie, Giardina, Bruland (b0220) 2015; 523 Mayor, Bautista, Bellot (b0145) 2011; 397 Ministry of Water Conservancy and Electric Power, PRC, 1956. Instructions for hydrometric station (in Chinese). Li, Zheng, Liu, Jiang (b0130) 2012; 82–83 Kimura, Liu, Takayama, Zhang, Kamichika, Matsuoka (b0120) 2005; 63 Fang, Shi, Chen, Zhang, Wang (b0065) 2015; 528 Parsons, Stone (b0180) 2006; 67 Zhao, Zhang, Chiew, Vaze, Cheng (b0285) 2013; 493 López-Tarazón, Batalla, Vericat, Balasch (b0140) 2010; 82 Chen (b0025) 2001; 11 Ran, Su, Li, He (b0205) 2012; 424–425 Zhou, Wang (b0330) 1992; 6 Faurès, Goodrich, Woolhiser, Sorooshian (b0075) 1995; 173 Zhang, Gao, Li, Tian (b0275) 2016; 80 Dou, Huang, Hong (b0030) 2009; 23 Guo, Duan (b0105) 2001 Fang, Chen, Cai, Li (b0050) 2007; 52 An, Zheng, Han (b0010) 2014; 179 Li, Li, Han, Li (b0125) 2009; 105 Yan, Yuan, Lei, Lei, Zhang, Su (b0260) 2014; 45 Ahmed, Rudra, Gharabaghi, Mackenzie, Dickinson (b0005) 2012 Shu, Liu, Yi, Zhang (b0215) 2008; 23 R Mkens, Helming, Prasad (b0200) 2002; 46 Fang, Cai, Li (b0045) 2009; 28 Paschalis, Fatichi, Molnar, Rimkus, Burlando (b0185) 2014; 514 Torri, Regüés, Pellegrini, Bazzoffi (b0230) 1999; 38 Zheng, Li, He (b0305) 2015; 29 Zheng, Qin, Yang, Cai (b0315) 2013; 109 Mu, Zhang, McVicar, Chille, Gau (b0170) 2007; 21 Fang, Cai, Chen, Li (b0060) 2008; 33 Suhaila, Jemain, Hamdan, Wan Zin (b0225) 2011; 411 Shen, Chen, Liao, Liu, Hong (b0210) 2012; 472–473 Yan (b0265) 1984 Frauenfeld, Truman (b0085) 2004; 169 Ministry of Water Conservancy and Electric Power, PRC, 1955. Tentative specification of hydrometric station (in Chinese). Zoccatelli, Borga, Zanon, Antonescu, Stancalie (b0335) 2010; 394 Dunkerley (b0035) 2012; 26 Peng, Wang (b0195) 2012; 90 Yellow River Conservancy Commission, Ministry of Water Conservancy and Electric Power, PRC, 1961–1971. Observed Data of Rainfall, Runoff and Sediment in the Zizhou Experimental Office over the Period 1959–1969 (in Chinese). Flanagan, Foster, Moldenhauer (b0080) 1988; 31 Zheng, Qin, Sun, Qi, Cai (b0310) 2011; 36 Zheng, Yang, Qi, Sun, Cai (b0320) 2012; 98 Zhao, Wu, Huang, Zhang, Gao (b0290) 2015; 24 Ouarda, Charron, Niranjan Kumar, Marpu, Ghedira, Molini, Khayal (b0175) 2014; 514 Guo, Yu, Fu, Li (b0100) 2014; 20 Liu, Nearing, Shi, Jia (b0135) 2000; 64 Wei, Chen, Fu (b0245) 2009; 33 Wang (b0235) 1991 Zheng, Cai, Cheng (b0300) 2008; 93 Hicks, Gomez, Trustrum (b0115) 2000; 36 Zhang (10.1016/j.jhydrol.2016.01.061_b0280) 2015; 31 Kimura (10.1016/j.jhydrol.2016.01.061_b0120) 2005; 63 Fang (10.1016/j.jhydrol.2016.01.061_b0045) 2009; 28 Gao (10.1016/j.jhydrol.2016.01.061_b0095) 2013; 29 Zhou (10.1016/j.jhydrol.2016.01.061_b0325) 1997; 4 Frauenfeld (10.1016/j.jhydrol.2016.01.061_b0085) 2004; 169 10.1016/j.jhydrol.2016.01.061_b0155 10.1016/j.jhydrol.2016.01.061_b0150 Dunkerley (10.1016/j.jhydrol.2016.01.061_b0035) 2012; 26 10.1016/j.jhydrol.2016.01.061_b0160 Dou (10.1016/j.jhydrol.2016.01.061_b0030) 2009; 23 An (10.1016/j.jhydrol.2016.01.061_b0010) 2014; 179 Yan (10.1016/j.jhydrol.2016.01.061_b0260) 2014; 45 Fang (10.1016/j.jhydrol.2016.01.061_b0055) 2008; 42 Xu (10.1016/j.jhydrol.2016.01.061_b0255) 1999; 36 Gao (10.1016/j.jhydrol.2016.01.061_b0090) 2015; 29 Zhao (10.1016/j.jhydrol.2016.01.061_b0290) 2015; 24 Guo (10.1016/j.jhydrol.2016.01.061_b0100) 2014; 20 Faurès (10.1016/j.jhydrol.2016.01.061_b0075) 1995; 173 Mayor (10.1016/j.jhydrol.2016.01.061_b0145) 2011; 397 Mu (10.1016/j.jhydrol.2016.01.061_b0170) 2007; 21 Zheng (10.1016/j.jhydrol.2016.01.061_b0310) 2011; 36 Parsons (10.1016/j.jhydrol.2016.01.061_b0180) 2006; 67 Wang (10.1016/j.jhydrol.2016.01.061_b0235) 1991 Li (10.1016/j.jhydrol.2016.01.061_b0125) 2009; 105 Ouarda (10.1016/j.jhydrol.2016.01.061_b0175) 2014; 514 Shen (10.1016/j.jhydrol.2016.01.061_b0210) 2012; 472–473 Zoccatelli (10.1016/j.jhydrol.2016.01.061_b0335) 2010; 394 R Mkens (10.1016/j.jhydrol.2016.01.061_b0200) 2002; 46 Hicks (10.1016/j.jhydrol.2016.01.061_b0115) 2000; 36 Yan (10.1016/j.jhydrol.2016.01.061_b0265) 1984 Li (10.1016/j.jhydrol.2016.01.061_b0130) 2012; 82–83 Ran (10.1016/j.jhydrol.2016.01.061_b0205) 2012; 424–425 Wei (10.1016/j.jhydrol.2016.01.061_b0245) 2009; 33 Zheng (10.1016/j.jhydrol.2016.01.061_b0315) 2013; 109 Strauch (10.1016/j.jhydrol.2016.01.061_b0220) 2015; 523 10.1016/j.jhydrol.2016.01.061_b0250 Cai (10.1016/j.jhydrol.2016.01.061_b0015) 2004; 23 Wei (10.1016/j.jhydrol.2016.01.061_b0240) 2007; 335 Fang (10.1016/j.jhydrol.2016.01.061_b0060) 2008; 33 Hancock (10.1016/j.jhydrol.2016.01.061_b0110) 2009; 152 Emmanuel (10.1016/j.jhydrol.2016.01.061_b0040) 2015; 531 Paschalis (10.1016/j.jhydrol.2016.01.061_b0185) 2014; 514 Zheng (10.1016/j.jhydrol.2016.01.061_b0320) 2012; 98 Zhang (10.1016/j.jhydrol.2016.01.061_b0275) 2016; 80 López-Tarazón (10.1016/j.jhydrol.2016.01.061_b0140) 2010; 82 Fang (10.1016/j.jhydrol.2016.01.061_b0070) 2012; 99 Ahmed (10.1016/j.jhydrol.2016.01.061_b0005) 2012 Zheng (10.1016/j.jhydrol.2016.01.061_b0305) 2015; 29 Shu (10.1016/j.jhydrol.2016.01.061_b0215) 2008; 23 Zhou (10.1016/j.jhydrol.2016.01.061_b0330) 1992; 6 Cammeraat (10.1016/j.jhydrol.2016.01.061_b0020) 2004; 104 Liu (10.1016/j.jhydrol.2016.01.061_b0135) 2000; 64 Peng (10.1016/j.jhydrol.2016.01.061_b0195) 2012; 90 Torri (10.1016/j.jhydrol.2016.01.061_b0230) 1999; 38 Guo (10.1016/j.jhydrol.2016.01.061_b0105) 2001 Flanagan (10.1016/j.jhydrol.2016.01.061_b0080) 1988; 31 Morin (10.1016/j.jhydrol.2016.01.061_b0165) 2006; 29 Suhaila (10.1016/j.jhydrol.2016.01.061_b0225) 2011; 411 Zheng (10.1016/j.jhydrol.2016.01.061_b0295) 2015; 10 Fang (10.1016/j.jhydrol.2016.01.061_b0050) 2007; 52 10.1016/j.jhydrol.2016.01.061_b0270 Zheng (10.1016/j.jhydrol.2016.01.061_b0300) 2008; 93 Chen (10.1016/j.jhydrol.2016.01.061_b0025) 2001; 11 Fang (10.1016/j.jhydrol.2016.01.061_b0065) 2015; 528 Zhao (10.1016/j.jhydrol.2016.01.061_b0285) 2013; 493
References_xml	– volume: 67 start-page: 68 year: 2006 end-page: 78 ident: b0180 article-title: Effects of intra-storm variations in rainfall intensity on interrill runoff and erosion publication-title: Catena – volume: 80 start-page: 775 year: 2016 end-page: 796 ident: b0275 article-title: Downslope runoff and erosion response of typical engineered landform to variable inflow rate patterns from upslope publication-title: Nat. Hazards – volume: 6 start-page: 1 year: 1992 end-page: 5 ident: b0330 article-title: A study on rainstorm causing soil erosion in the Loess Plateau publication-title: J. Soil Water Conserv. – reference: Williams, J.R., 1975. Sediment-yield prediction with universal equation using runoff energy factor. In: Present and Pro-spective Technology for Predicting Sediment Yield and Sources. Proceedings of the Sediment-yield Workshop, USDA Sedimentation Lab., Oxford, MS, November 28–30, 1972. ARS-S-40, pp. 244–252. – year: 1984 ident: b0265 article-title: An Introduction to Hydrometry – volume: 10 start-page: e0117989 year: 2015 ident: b0295 article-title: Statistical determination of rainfall-runoff erosivity indices for single storms in the Chinese Loess Plateau publication-title: PLoS ONE – volume: 64 start-page: 1759 year: 2000 end-page: 1763 ident: b0135 article-title: Slope length effects on soil loss for steep slopes publication-title: Soil Sci. Soc. Am. J. – year: 1991 ident: b0235 article-title: Dataset by Remote Sense for Resource and Environment in the Loess Plateau Region – volume: 493 start-page: 16 year: 2013 end-page: 29 ident: b0285 article-title: The effect of spatial rainfall variability on water balance modelling for south-eastern Australian catchments publication-title: J. Hydrol. – volume: 397 start-page: 128 year: 2011 end-page: 135 ident: b0145 article-title: Scale-dependent variation in runoff and sediment yield in a semiarid Mediterranean catchment publication-title: J. Hydrol. – volume: 38 start-page: 131 year: 1999 end-page: 150 ident: b0230 article-title: Within-storm soil surface dynamics and erosive effects of rainstorms publication-title: Catena – volume: 42 start-page: 402 year: 2008 end-page: 411 ident: b0055 article-title: Effect of rainfall regime and slope on runoff in a gullied loess region on the Loess Plateau in China publication-title: Environ. Manage. – volume: 36 start-page: 1 year: 1999 end-page: 19 ident: b0255 article-title: Erosion caused by hyperconcentrated flow on the Loess Plateau of China publication-title: Catena – volume: 424–425 start-page: 99 year: 2012 end-page: 111 ident: b0205 article-title: Experimental study of the impact of rainfall characteristics on runoff generation and soil erosion publication-title: J. Hydrol. – year: 2012 ident: b0005 article-title: Within-storm rainfall distribution effect on soil erosion rate publication-title: ISRN Soil Sci. – volume: 33 start-page: 1 year: 2009 end-page: 12 ident: b0245 article-title: Effects of rainfall change on water erosion processes in terrestrial ecosystems: a review publication-title: Prog. Phys. Geogr. – volume: 52 start-page: 753 year: 2007 end-page: 760 ident: b0050 article-title: Scale effect on sediment yield from sloping surfaces to basins in hilly loess region on the Loess Plateau in China publication-title: Environ. Geol. – volume: 179 start-page: 293 year: 2014 end-page: 303 ident: b0010 article-title: Effects of rainstorm patterns on runoff and sediment yield processes publication-title: Soil Sci. – volume: 29 start-page: 843 year: 2006 end-page: 860 ident: b0165 article-title: Spatial patterns in thunderstorm rainfall events and their coupling with watershed hydrological response publication-title: Adv. Water Resour. – volume: 21 start-page: 2124 year: 2007 end-page: 2134 ident: b0170 article-title: Analysis of the impact of conservation measures on stream flow regime in catchments of the Loess Plateau, China publication-title: Hydrol. Process. – volume: 63 start-page: 439 year: 2005 end-page: 457 ident: b0120 article-title: Heat and water balances of the bare soil surface and the potential distribution of vegetation in the Loess Plateau, China publication-title: J. Arid Environ. – volume: 29 start-page: 5414 year: 2015 end-page: 5423 ident: b0305 article-title: Sediment concentrations in run-off varying with spatial scale in an agricultural subwatershed of the Chinese Loess Plateau publication-title: Hydrol. Process. – volume: 98 start-page: 29 year: 2012 end-page: 40 ident: b0320 article-title: Flow–sediment relationship as functions of spatial and temporal scales in hilly areas of the Chinese Loess Plateau publication-title: Catena – volume: 82–83 start-page: 65 year: 2012 end-page: 73 ident: b0130 article-title: Spatially downscaling GCMs outputs to project changes in extreme precipitation and temperature events on the Loess Plateau of China during the 21st Century publication-title: Global Planet. Change – reference: Ministry of Water Conservancy and Electric Power, PRC, 1955. Tentative specification of hydrometric station (in Chinese). – volume: 93 start-page: 288 year: 2008 end-page: 301 ident: b0300 article-title: Modelling the runoff–sediment yield relationship using a proportional function in hilly areas of the Loess Plateau, North China publication-title: Geomorphology – volume: 24 start-page: 32 year: 2015 end-page: 38 ident: b0290 article-title: Review of applied basis research on regulation and utilization of rainfall runoff in Loess Plateau of China publication-title: J. Nat. Disasters – volume: 394 start-page: 148 year: 2010 end-page: 161 ident: b0335 article-title: Which rainfall spatial information for flash flood response modelling? A numerical investigation based on data from the Carpathian range, Romania publication-title: J. Hydrol. – volume: 531 start-page: 337 year: 2015 end-page: 348 ident: b0040 article-title: Influence of rainfall spatial variability on rainfall–runoff modelling: benefit of a simulation approach? publication-title: J. Hydrol. – volume: 31 start-page: 414 year: 1988 end-page: 420 ident: b0080 article-title: Storm pattern effect on infiltration, runoff and erosion publication-title: Trans. ASAE – volume: 29 start-page: 2402 year: 2015 end-page: 2413 ident: b0090 article-title: Streamflow regimes of the Yanhe River under climate and land use change, Loess Plateau, China publication-title: Hydrol. Process. – volume: 109 start-page: 164 year: 2013 end-page: 176 ident: b0315 article-title: The spatio-temporal invariability of sediment concentration and the flow–sediment relationship for hilly areas of the Chinese Loess Plateau publication-title: Catena – volume: 20 start-page: C4014011 year: 2014 ident: b0100 article-title: Improved Hillslope erosion module for the digital yellow-river model publication-title: J. Hydrol. Eng. – start-page: 1 year: 2001 end-page: 5 ident: b0105 article-title: The theory of runoff regulation and control is the quintessence of soil and water conservation: the fourth discussion on the unique characteristics of soil and water conservation publication-title: Soil Water Conserv. China – volume: 26 start-page: 2211 year: 2012 end-page: 2224 ident: b0035 article-title: Effects of rainfall intensity fluctuations on infiltration and runoff: rainfall simulation on dryland soils, Fowlers Gap, Australia publication-title: Hydrol. Process. – volume: 28 start-page: 583 year: 2009 end-page: 591 ident: b0045 article-title: Study on the runoff generation capacity of slope surface and its influencing factors in a hilly loess region on the Loess Plateau publication-title: Geogr. Res. – volume: 472–473 start-page: 205 year: 2012 end-page: 215 ident: b0210 article-title: Impact of spatial rainfall variability on hydrology and nonpoint source pollution modeling publication-title: J. Hydrol. – volume: 23 start-page: 1935 year: 2009 end-page: 1949 ident: b0030 article-title: Statistical assessment of the impact of conservation measures on streamflow responses in a watershed of the Loess Plateau, China publication-title: Water Resour. Manage. – volume: 36 start-page: 1499 year: 2011 end-page: 1509 ident: b0310 article-title: Spatial scale effects on sediment concentration in runoff during flood events for hilly areas of the Loess Plateau, China publication-title: Earth Surf. Proc. Land. – volume: 99 start-page: 1 year: 2012 end-page: 8 ident: b0070 article-title: The effects of rainfall regimes and land use changes on runoff and soil loss in a small mountainous watershed publication-title: Catena – volume: 523 start-page: 160 year: 2015 end-page: 169 ident: b0220 article-title: Climate driven changes to rainfall and streamflow patterns in a model tropical island hydrological system publication-title: J. Hydrol. – reference: Ministry of Water Conservancy and Electric Power, PRC, 1975. Tentative specification of hydrometry (in Chinese). – volume: 411 start-page: 197 year: 2011 end-page: 206 ident: b0225 article-title: Comparing rainfall patterns between regions in Peninsular Malaysia via a functional data analysis technique publication-title: J. Hydrol. – volume: 45 start-page: 169 year: 2014 end-page: 175 ident: b0260 article-title: Effect of rainstorm patterns and soil erosion control practices on soil and water loss in small watershed on Loess Plateau publication-title: Trans. Chin. Soc. Agric. Mach. – volume: 11 start-page: 71 year: 2001 end-page: 79 ident: b0025 article-title: Relationship between erosion and sediment yield in drainage basins of loess gully-hilly areas publication-title: J. Geog. Sci. – volume: 173 start-page: 309 year: 1995 end-page: 326 ident: b0075 article-title: Impact of small-scale spatial rainfall variability on runoff modeling publication-title: J. Hydrol. – volume: 23 start-page: 387 year: 2008 end-page: 397 ident: b0215 article-title: Characteristics of energy dissipation in hyperconcentrated flows publication-title: Int. J. Sedim. Res. – volume: 335 start-page: 247 year: 2007 end-page: 258 ident: b0240 article-title: The effect of land uses and rainfall regimes on runoff and soil erosion in the semi-arid loess hilly area, China publication-title: J. Hydrol. – volume: 46 start-page: 103 year: 2002 end-page: 123 ident: b0200 article-title: Soil erosion under different rainfall intensities, surface roughness, and soil water regimes publication-title: Catena – volume: 33 start-page: 1977 year: 2008 end-page: 1992 ident: b0060 article-title: Temporal changes in suspended sediment transport in a gullied loess basin: the lower Chabagou Creek on the Loess Plateau in China publication-title: Earth Surf. Proc. Land. – volume: 82 start-page: 23 year: 2010 end-page: 34 ident: b0140 article-title: Rainfall, runoff and sediment transport relations in a mesoscale mountainous catchment: the River Isábena (Ebro basin) publication-title: Catena – volume: 514 start-page: 313 year: 2014 end-page: 327 ident: b0185 article-title: On the effects of small scale space–time variability of rainfall on basin flood response publication-title: J. Hydrol. – volume: 105 start-page: 285 year: 2009 end-page: 291 ident: b0125 article-title: Sediment flow behavior in agro-watersheds of the purple soil region in China under different storm types and spatial scales publication-title: Soil Tillage Res. – volume: 29 start-page: 99 year: 2013 end-page: 105 ident: b0095 article-title: Responses of streamflow and sediment load to vegetation restoration in catchments on the Loess Plateau publication-title: Trans. CSAE – reference: Yellow River Conservancy Commission, Ministry of Water Conservancy and Electric Power, PRC, 1961–1971. Observed Data of Rainfall, Runoff and Sediment in the Zizhou Experimental Office over the Period 1959–1969 (in Chinese). – volume: 31 start-page: 124 year: 2015 end-page: 131 ident: b0280 article-title: Impact of runoff regimes on sediment yield and sediment flow behavior at slope scale publication-title: Trans. CSAE – volume: 4 start-page: 40 year: 1997 end-page: 46 ident: b0325 article-title: Discussion on mechanism of loess erosion publication-title: Res. Soil Water Conserv. – volume: 23 start-page: 433 year: 2004 end-page: 439 ident: b0015 article-title: Research of sediment yield statistical model for single rainstorm in Chabagou drainage basin publication-title: Geogr. Res. – volume: 104 start-page: 317 year: 2004 end-page: 332 ident: b0020 article-title: Scale dependent thresholds in hydrological and erosion response of a semi-arid catchment in southeast Spain publication-title: Agric. Ecosyst. Environ. – volume: 169 start-page: 143 year: 2004 end-page: 154 ident: b0085 article-title: Variable rainfall intensity effects on runoff and interrill erosion from two Coastal Plain Ultisols in Georgia publication-title: Soil Sci. – volume: 36 start-page: 1129 year: 2000 end-page: 1142 ident: b0115 article-title: Erosion thresholds and suspended sediment yields, Waipaoa River basin, New Zealand publication-title: Water Resour. Res. – volume: 90 start-page: 53 year: 2012 end-page: 62 ident: b0195 article-title: Effects of land use, land cover and rainfall regimes on the surface runoff and soil loss on karst slopes in southwest China publication-title: Catena – volume: 528 start-page: 238 year: 2015 end-page: 248 ident: b0065 article-title: Discharge and suspended sediment patterns in a small mountainous watershed with widely distributed rock fragments publication-title: J. Hydrol. – volume: 514 start-page: 258 year: 2014 end-page: 270 ident: b0175 article-title: Evolution of the rainfall regime in the United Arab Emirates publication-title: J. Hydrol. – volume: 152 start-page: 350 year: 2009 end-page: 360 ident: b0110 article-title: A catchment scale assessment of increased rainfall and storm intensity on erosion and sediment transport for Northern Australia publication-title: Geoderma – reference: Ministry of Water Conservancy and Electric Power, PRC, 1956. Instructions for hydrometric station (in Chinese). – volume: 24 start-page: 32 issue: 1 year: 2015 ident: 10.1016/j.jhydrol.2016.01.061_b0290 article-title: Review of applied basis research on regulation and utilization of rainfall runoff in Loess Plateau of China publication-title: J. Nat. Disasters – volume: 36 start-page: 1499 issue: 11 year: 2011 ident: 10.1016/j.jhydrol.2016.01.061_b0310 article-title: Spatial scale effects on sediment concentration in runoff during flood events for hilly areas of the Loess Plateau, China publication-title: Earth Surf. Proc. Land. doi: 10.1002/esp.2176 – volume: 31 start-page: 414 issue: 2 year: 1988 ident: 10.1016/j.jhydrol.2016.01.061_b0080 article-title: Storm pattern effect on infiltration, runoff and erosion publication-title: Trans. ASAE doi: 10.13031/2013.30724 – volume: 173 start-page: 309 year: 1995 ident: 10.1016/j.jhydrol.2016.01.061_b0075 article-title: Impact of small-scale spatial rainfall variability on runoff modeling publication-title: J. Hydrol. doi: 10.1016/0022-1694(95)02704-S – volume: 42 start-page: 402 issue: 3 year: 2008 ident: 10.1016/j.jhydrol.2016.01.061_b0055 article-title: Effect of rainfall regime and slope on runoff in a gullied loess region on the Loess Plateau in China publication-title: Environ. Manage. doi: 10.1007/s00267-008-9122-6 – volume: 105 start-page: 285 issue: 2 year: 2009 ident: 10.1016/j.jhydrol.2016.01.061_b0125 article-title: Sediment flow behavior in agro-watersheds of the purple soil region in China under different storm types and spatial scales publication-title: Soil Tillage Res. doi: 10.1016/j.still.2009.04.002 – volume: 29 start-page: 2402 year: 2015 ident: 10.1016/j.jhydrol.2016.01.061_b0090 article-title: Streamflow regimes of the Yanhe River under climate and land use change, Loess Plateau, China publication-title: Hydrol. Process. doi: 10.1002/hyp.10309 – volume: 52 start-page: 753 issue: 4 year: 2007 ident: 10.1016/j.jhydrol.2016.01.061_b0050 article-title: Scale effect on sediment yield from sloping surfaces to basins in hilly loess region on the Loess Plateau in China publication-title: Environ. Geol. doi: 10.1007/s00254-006-0513-9 – volume: 528 start-page: 238 year: 2015 ident: 10.1016/j.jhydrol.2016.01.061_b0065 article-title: Discharge and suspended sediment patterns in a small mountainous watershed with widely distributed rock fragments publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2015.06.046 – volume: 21 start-page: 2124 issue: 16 year: 2007 ident: 10.1016/j.jhydrol.2016.01.061_b0170 article-title: Analysis of the impact of conservation measures on stream flow regime in catchments of the Loess Plateau, China publication-title: Hydrol. Process. doi: 10.1002/hyp.6391 – volume: 29 start-page: 5414 issue: 26 year: 2015 ident: 10.1016/j.jhydrol.2016.01.061_b0305 article-title: Sediment concentrations in run-off varying with spatial scale in an agricultural subwatershed of the Chinese Loess Plateau publication-title: Hydrol. Process. doi: 10.1002/hyp.10576 – volume: 45 start-page: 169 issue: 2 year: 2014 ident: 10.1016/j.jhydrol.2016.01.061_b0260 article-title: Effect of rainstorm patterns and soil erosion control practices on soil and water loss in small watershed on Loess Plateau publication-title: Trans. Chin. Soc. Agric. Mach. – volume: 4 start-page: 40 issue: 5 year: 1997 ident: 10.1016/j.jhydrol.2016.01.061_b0325 article-title: Discussion on mechanism of loess erosion publication-title: Res. Soil Water Conserv. – volume: 152 start-page: 350 year: 2009 ident: 10.1016/j.jhydrol.2016.01.061_b0110 article-title: A catchment scale assessment of increased rainfall and storm intensity on erosion and sediment transport for Northern Australia publication-title: Geoderma doi: 10.1016/j.geoderma.2009.07.003 – volume: 424–425 start-page: 99 year: 2012 ident: 10.1016/j.jhydrol.2016.01.061_b0205 article-title: Experimental study of the impact of rainfall characteristics on runoff generation and soil erosion publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2011.12.035 – volume: 64 start-page: 1759 issue: 5 year: 2000 ident: 10.1016/j.jhydrol.2016.01.061_b0135 article-title: Slope length effects on soil loss for steep slopes publication-title: Soil Sci. Soc. Am. J. doi: 10.2136/sssaj2000.6451759x – volume: 514 start-page: 313 year: 2014 ident: 10.1016/j.jhydrol.2016.01.061_b0185 article-title: On the effects of small scale space–time variability of rainfall on basin flood response publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2014.04.014 – volume: 23 start-page: 433 issue: 4 year: 2004 ident: 10.1016/j.jhydrol.2016.01.061_b0015 article-title: Research of sediment yield statistical model for single rainstorm in Chabagou drainage basin publication-title: Geogr. Res. – year: 2012 ident: 10.1016/j.jhydrol.2016.01.061_b0005 article-title: Within-storm rainfall distribution effect on soil erosion rate publication-title: ISRN Soil Sci. doi: 10.5402/2012/310927 – volume: 33 start-page: 1977 issue: 13 year: 2008 ident: 10.1016/j.jhydrol.2016.01.061_b0060 article-title: Temporal changes in suspended sediment transport in a gullied loess basin: the lower Chabagou Creek on the Loess Plateau in China publication-title: Earth Surf. Proc. Land. doi: 10.1002/esp.1649 – start-page: 1 issue: 11 year: 2001 ident: 10.1016/j.jhydrol.2016.01.061_b0105 article-title: The theory of runoff regulation and control is the quintessence of soil and water conservation: the fourth discussion on the unique characteristics of soil and water conservation publication-title: Soil Water Conserv. China – volume: 411 start-page: 197 year: 2011 ident: 10.1016/j.jhydrol.2016.01.061_b0225 article-title: Comparing rainfall patterns between regions in Peninsular Malaysia via a functional data analysis technique publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2011.09.043 – volume: 82 start-page: 23 year: 2010 ident: 10.1016/j.jhydrol.2016.01.061_b0140 article-title: Rainfall, runoff and sediment transport relations in a mesoscale mountainous catchment: the River Isábena (Ebro basin) publication-title: Catena doi: 10.1016/j.catena.2010.04.005 – volume: 33 start-page: 1 issue: 3 year: 2009 ident: 10.1016/j.jhydrol.2016.01.061_b0245 article-title: Effects of rainfall change on water erosion processes in terrestrial ecosystems: a review publication-title: Prog. Phys. Geogr. doi: 10.1177/0309133309341426 – volume: 10 start-page: e0117989 issue: 3 year: 2015 ident: 10.1016/j.jhydrol.2016.01.061_b0295 article-title: Statistical determination of rainfall-runoff erosivity indices for single storms in the Chinese Loess Plateau publication-title: PLoS ONE doi: 10.1371/journal.pone.0117989 – volume: 82–83 start-page: 65 year: 2012 ident: 10.1016/j.jhydrol.2016.01.061_b0130 article-title: Spatially downscaling GCMs outputs to project changes in extreme precipitation and temperature events on the Loess Plateau of China during the 21st Century publication-title: Global Planet. Change doi: 10.1016/j.gloplacha.2011.11.008 – volume: 394 start-page: 148 year: 2010 ident: 10.1016/j.jhydrol.2016.01.061_b0335 article-title: Which rainfall spatial information for flash flood response modelling? A numerical investigation based on data from the Carpathian range, Romania publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2010.07.019 – volume: 67 start-page: 68 year: 2006 ident: 10.1016/j.jhydrol.2016.01.061_b0180 article-title: Effects of intra-storm variations in rainfall intensity on interrill runoff and erosion publication-title: Catena doi: 10.1016/j.catena.2006.03.002 – volume: 36 start-page: 1129 issue: 4 year: 2000 ident: 10.1016/j.jhydrol.2016.01.061_b0115 article-title: Erosion thresholds and suspended sediment yields, Waipaoa River basin, New Zealand publication-title: Water Resour. Res. doi: 10.1029/1999WR900340 – volume: 20 start-page: C4014011 issue: 6 year: 2014 ident: 10.1016/j.jhydrol.2016.01.061_b0100 article-title: Improved Hillslope erosion module for the digital yellow-river model publication-title: J. Hydrol. Eng. doi: 10.1061/(ASCE)HE.1943-5584.0001117 – ident: 10.1016/j.jhydrol.2016.01.061_b0250 – volume: 104 start-page: 317 issue: 2 year: 2004 ident: 10.1016/j.jhydrol.2016.01.061_b0020 article-title: Scale dependent thresholds in hydrological and erosion response of a semi-arid catchment in southeast Spain publication-title: Agric. Ecosyst. Environ. doi: 10.1016/j.agee.2004.01.032 – volume: 397 start-page: 128 issue: 1–2 year: 2011 ident: 10.1016/j.jhydrol.2016.01.061_b0145 article-title: Scale-dependent variation in runoff and sediment yield in a semiarid Mediterranean catchment publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2010.11.039 – volume: 46 start-page: 103 year: 2002 ident: 10.1016/j.jhydrol.2016.01.061_b0200 article-title: Soil erosion under different rainfall intensities, surface roughness, and soil water regimes publication-title: Catena doi: 10.1016/S0341-8162(01)00161-8 – volume: 493 start-page: 16 year: 2013 ident: 10.1016/j.jhydrol.2016.01.061_b0285 article-title: The effect of spatial rainfall variability on water balance modelling for south-eastern Australian catchments publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2013.04.028 – year: 1991 ident: 10.1016/j.jhydrol.2016.01.061_b0235 – volume: 11 start-page: 71 issue: 1 year: 2001 ident: 10.1016/j.jhydrol.2016.01.061_b0025 article-title: Relationship between erosion and sediment yield in drainage basins of loess gully-hilly areas publication-title: J. Geog. Sci. doi: 10.1007/BF02837377 – ident: 10.1016/j.jhydrol.2016.01.061_b0160 – volume: 179 start-page: 293 issue: 6 year: 2014 ident: 10.1016/j.jhydrol.2016.01.061_b0010 article-title: Effects of rainstorm patterns on runoff and sediment yield processes publication-title: Soil Sci. doi: 10.1097/SS.0000000000000068 – volume: 31 start-page: 124 issue: 20 year: 2015 ident: 10.1016/j.jhydrol.2016.01.061_b0280 article-title: Impact of runoff regimes on sediment yield and sediment flow behavior at slope scale publication-title: Trans. CSAE – volume: 23 start-page: 387 issue: 4 year: 2008 ident: 10.1016/j.jhydrol.2016.01.061_b0215 article-title: Characteristics of energy dissipation in hyperconcentrated flows publication-title: Int. J. Sedim. Res. doi: 10.1016/S1001-6279(09)60009-3 – year: 1984 ident: 10.1016/j.jhydrol.2016.01.061_b0265 – volume: 90 start-page: 53 year: 2012 ident: 10.1016/j.jhydrol.2016.01.061_b0195 article-title: Effects of land use, land cover and rainfall regimes on the surface runoff and soil loss on karst slopes in southwest China publication-title: Catena doi: 10.1016/j.catena.2011.11.001 – volume: 531 start-page: 337 year: 2015 ident: 10.1016/j.jhydrol.2016.01.061_b0040 article-title: Influence of rainfall spatial variability on rainfall–runoff modelling: benefit of a simulation approach? publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2015.04.058 – volume: 63 start-page: 439 issue: 2 year: 2005 ident: 10.1016/j.jhydrol.2016.01.061_b0120 article-title: Heat and water balances of the bare soil surface and the potential distribution of vegetation in the Loess Plateau, China publication-title: J. Arid Environ. doi: 10.1016/j.jaridenv.2005.03.030 – volume: 514 start-page: 258 year: 2014 ident: 10.1016/j.jhydrol.2016.01.061_b0175 article-title: Evolution of the rainfall regime in the United Arab Emirates publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2014.04.032 – volume: 38 start-page: 131 year: 1999 ident: 10.1016/j.jhydrol.2016.01.061_b0230 article-title: Within-storm soil surface dynamics and erosive effects of rainstorms publication-title: Catena doi: 10.1016/S0341-8162(99)00059-4 – volume: 80 start-page: 775 issue: 2 year: 2016 ident: 10.1016/j.jhydrol.2016.01.061_b0275 article-title: Downslope runoff and erosion response of typical engineered landform to variable inflow rate patterns from upslope publication-title: Nat. Hazards doi: 10.1007/s11069-015-1996-z – volume: 335 start-page: 247 year: 2007 ident: 10.1016/j.jhydrol.2016.01.061_b0240 article-title: The effect of land uses and rainfall regimes on runoff and soil erosion in the semi-arid loess hilly area, China publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2006.11.016 – volume: 98 start-page: 29 year: 2012 ident: 10.1016/j.jhydrol.2016.01.061_b0320 article-title: Flow–sediment relationship as functions of spatial and temporal scales in hilly areas of the Chinese Loess Plateau publication-title: Catena doi: 10.1016/j.catena.2012.05.013 – volume: 28 start-page: 583 issue: 3 year: 2009 ident: 10.1016/j.jhydrol.2016.01.061_b0045 article-title: Study on the runoff generation capacity of slope surface and its influencing factors in a hilly loess region on the Loess Plateau publication-title: Geogr. Res. – volume: 99 start-page: 1 year: 2012 ident: 10.1016/j.jhydrol.2016.01.061_b0070 article-title: The effects of rainfall regimes and land use changes on runoff and soil loss in a small mountainous watershed publication-title: Catena doi: 10.1016/j.catena.2012.07.004 – volume: 472–473 start-page: 205 year: 2012 ident: 10.1016/j.jhydrol.2016.01.061_b0210 article-title: Impact of spatial rainfall variability on hydrology and nonpoint source pollution modeling publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2012.09.019 – volume: 523 start-page: 160 year: 2015 ident: 10.1016/j.jhydrol.2016.01.061_b0220 article-title: Climate driven changes to rainfall and streamflow patterns in a model tropical island hydrological system publication-title: J. Hydrol. doi: 10.1016/j.jhydrol.2015.01.045 – volume: 26 start-page: 2211 issue: 15 year: 2012 ident: 10.1016/j.jhydrol.2016.01.061_b0035 article-title: Effects of rainfall intensity fluctuations on infiltration and runoff: rainfall simulation on dryland soils, Fowlers Gap, Australia publication-title: Hydrol. Process. doi: 10.1002/hyp.8317 – ident: 10.1016/j.jhydrol.2016.01.061_b0150 – ident: 10.1016/j.jhydrol.2016.01.061_b0155 – volume: 29 start-page: 99 issue: 6 year: 2013 ident: 10.1016/j.jhydrol.2016.01.061_b0095 article-title: Responses of streamflow and sediment load to vegetation restoration in catchments on the Loess Plateau publication-title: Trans. CSAE – volume: 109 start-page: 164 year: 2013 ident: 10.1016/j.jhydrol.2016.01.061_b0315 article-title: The spatio-temporal invariability of sediment concentration and the flow–sediment relationship for hilly areas of the Chinese Loess Plateau publication-title: Catena doi: 10.1016/j.catena.2013.03.017 – volume: 36 start-page: 1 year: 1999 ident: 10.1016/j.jhydrol.2016.01.061_b0255 article-title: Erosion caused by hyperconcentrated flow on the Loess Plateau of China publication-title: Catena doi: 10.1016/S0341-8162(99)00009-0 – ident: 10.1016/j.jhydrol.2016.01.061_b0270 – volume: 23 start-page: 1935 issue: 10 year: 2009 ident: 10.1016/j.jhydrol.2016.01.061_b0030 article-title: Statistical assessment of the impact of conservation measures on streamflow responses in a watershed of the Loess Plateau, China publication-title: Water Resour. Manage. doi: 10.1007/s11269-008-9361-6 – volume: 6 start-page: 1 issue: 3 year: 1992 ident: 10.1016/j.jhydrol.2016.01.061_b0330 article-title: A study on rainstorm causing soil erosion in the Loess Plateau publication-title: J. Soil Water Conserv. – volume: 169 start-page: 143 issue: 2 year: 2004 ident: 10.1016/j.jhydrol.2016.01.061_b0085 article-title: Variable rainfall intensity effects on runoff and interrill erosion from two Coastal Plain Ultisols in Georgia publication-title: Soil Sci. doi: 10.1097/01.ss.0000117784.98510.46 – volume: 93 start-page: 288 year: 2008 ident: 10.1016/j.jhydrol.2016.01.061_b0300 article-title: Modelling the runoff–sediment yield relationship using a proportional function in hilly areas of the Loess Plateau, North China publication-title: Geomorphology doi: 10.1016/j.geomorph.2007.03.001 – volume: 29 start-page: 843 issue: 6 year: 2006 ident: 10.1016/j.jhydrol.2016.01.061_b0165 article-title: Spatial patterns in thunderstorm rainfall events and their coupling with watershed hydrological response publication-title: Adv. Water Resour. doi: 10.1016/j.advwatres.2005.07.014
SSID	ssj0000334
Score	2.3816652
Snippet	[Display omitted] •Intra event-based flood regimes were analyzed at catchment scale.•Sediment flow behavior under different flood regimes was... The pluvial erosion process is significantly affected by tempo-spatial patterns of flood flows. However, despite their importance, only a few studies have...
SourceID	proquest crossref elsevier
SourceType	Aggregation Database Enrichment Source Index Database Publisher
StartPage	71
SubjectTerms	agricultural watersheds analysis of variance Catchments China discriminant analysis Dynamics energy equations Exports Flood regime Floods Freshwater Hierarchical clustering approach Internal sediment reduction International trade loess Mathematical analysis Runoff Runoff self-regulation mechanism Sediment flow behavior sediment transport sediment yield Sediments soil soil erosion suspended sediment
Title	Influence of intra-event-based flood regime on sediment flow behavior from a typical agro-catchment of the Chinese Loess Plateau
URI	https://dx.doi.org/10.1016/j.jhydrol.2016.01.061 https://www.proquest.com/docview/1808699001 https://www.proquest.com/docview/1825426301 https://www.proquest.com/docview/1825472324
Volume	538
WOSCitedRecordID	wos000378360600007&url=https%3A%2F%2Fcvtisr.summon.serialssolutions.com%2F%23%21%2Fsearch%3Fho%3Df%26include.ft.matches%3Dt%26l%3Dnull%26q%3D
hasFullText	1
inHoldings	1
isFullTextHit
isPrint
journalDatabaseRights	– providerCode: PRVESC databaseName: Elsevier SD Freedom Collection Journals 2021 customDbUrl: eissn: 1879-2707 dateEnd: 99991231 omitProxy: false ssIdentifier: ssj0000334 issn: 0022-1694 databaseCode: AIEXJ dateStart: 19950101 isFulltext: true titleUrlDefault: https://www.sciencedirect.com providerName: Elsevier
link	http://cvtisr.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwtV1Lb9NAEF6FFgkuiKcoLy0S4hJtsbO21z4GlNKiKPSQQm6rtb2miVI75NGWG7-DX8uMd9cp0JJy4GJF-7CTzOeZ2d2Zbwh5FSoFVjcNGFjzDgsyeBVTjyvmpZ08LkBrRjUdw6e-GAzi0Sg5bLV-uFyY06koy_j8PJn9V1FDGwgbU2f_QdzNTaEBPoPQ4Qpih-u1BH_gyo5YNoi5YjVLE0ODlbcLjFRvYz2GE40nBdBWE_xjx1mTtW_SThTu0Bo6gS_zimWgto9d8AA6rFh8Wy90u1-hvjycgt-qVle4u8ff8rnhewKftnuC_Aw5grHZiGi2rvuaDVXVRArV4QbYyd6OGyR_tmP3G1yOxsocIq1gYHVxM8OPmsDXi8kFfmTqHjsFHRr-F6tiTcUWZ6z9S82A2ZGY7E7Mb8MIvqhmZ438td1zZ_2Dj3LvqN-Xw95o-Hr2lWFFMjy5t-VZbpDtjggT0Jjb3YPe6MPaznMeOC56_Mrr_LA3lz75Ks_nNx-gdmyGd8kdKyLaNUi6R1q6vE9uvdeWy_wB-d4gilYF_QNRtEYUNYiiVUkdorDjjDpEUUQUVdQiiv6KKLwzIIpaRNEaUdQi6iE52usN3-0zW7iDKfBHlwxWqSmPcWULeoorrkOvo5WnijjNojBRuV8oTyReIpIwg_U3j0UaCe2LIlfgfyr-iGyVVakfExoUIs_yLEh5VARJESmuYt8r_DjlQugi2SGB-1NlZlntsbjKVLrwxYm0spAoC-n5EmSxQ3abaTND67JpQuwkJq1vanxOCZjbNPWlk7AE3Y0HcqrU1Woh_diLI3AHvb-O6YRYVGHjGIFroyfXGPOU3F6_es_I1nK-0s_Jzex0OV7MX1iU_wQjbNd2
linkProvider	Elsevier
openUrl	ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=Influence+of+intra-event-based+flood+regime+on+sediment+flow+behavior+from+a+typical+agro-catchment+of+the+Chinese+Loess+Plateau&rft.jtitle=Journal+of+hydrology+%28Amsterdam%29&rft.au=Zhang%2C+Le-Tao&rft.au=Li%2C+Zhan-Bin&rft.au=Wang%2C+He&rft.au=Xiao%2C+Jun-Bo&rft.date=2016-07-01&rft.issn=0022-1694&rft.volume=538&rft.spage=71&rft.epage=81&rft_id=info:doi/10.1016%2Fj.jhydrol.2016.01.061&rft.externalDBID=NO_FULL_TEXT
thumbnail_l	http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/lc.gif&issn=0022-1694&client=summon
thumbnail_m	http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/mc.gif&issn=0022-1694&client=summon
thumbnail_s	http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/sc.gif&issn=0022-1694&client=summon