Comparison of geostatistical and response surface methodology for estimating soil saturated hydraulic conductivity

Soil saturated hydraulic conductivity (Ks) is a critical parameter for modeling water and solute transport in soils. Conventional laboratory measurements of Ks are labor-intensive, costly, and susceptible to measurement errors, underscoring the need for more reliable estimation techniques. This stud...

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Vydáno v:	Scientific reports Ročník 15; číslo 1; s. 34103 - 14
Hlavní autor:	Cheng, Lin
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	London Nature Publishing Group UK 30.09.2025 Nature Publishing Group Nature Portfolio
Témata:	631/158 639/166 704/158 704/172 704/2151 704/242 Accuracy Agricultural management Co-kriging Environmental science Humanities and Social Sciences Hydraulics Hydrology Land use planning Machine learning multidisciplinary Neural networks Ordinary kriging Physicochemical properties Response surface methodology Salinity Saturated soils Science Science (multidisciplinary) Soil erosion Soil properties Soil saturated hydraulic conductivity Solute transport Support vector machines Water Water resources China Henan China Co-kriging Soil saturated hydraulic conductivity Response surface methodology Ordinary kriging
ISSN:	2045-2322, 2045-2322
On-line přístup:	Získat plný text
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