2023
DOI: 10.1016/j.catena.2022.106846
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Variations in the concentration, composition, and sources of WEOM in erosion and deposition landscapes over an erosion intensity gradient on the Loess Plateau of China

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Cited by 5 publications
(1 citation statement)
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“…In the case of dissolved organic carbon (DOC), its concentration is higher at the beginning of the runoff and later, if diluting occurs (Mchunu & Chaplot 2012). Water-extractable organic carbon (WEOC) is a part of DOC and it is the most active and mobile fraction of OC, which reacts very sensitively to water erosion, while more pronounced fluctuations in the WEOC contents are below 0.2 m (Yao et al 2023). Rizinjirabake et al (2019) did not observe more pronounced differences in the WEOC in the upper slopes, in concave and convex areas or places of topsoil accumulation conditioned by erosion.…”
mentioning
confidence: 99%
“…In the case of dissolved organic carbon (DOC), its concentration is higher at the beginning of the runoff and later, if diluting occurs (Mchunu & Chaplot 2012). Water-extractable organic carbon (WEOC) is a part of DOC and it is the most active and mobile fraction of OC, which reacts very sensitively to water erosion, while more pronounced fluctuations in the WEOC contents are below 0.2 m (Yao et al 2023). Rizinjirabake et al (2019) did not observe more pronounced differences in the WEOC in the upper slopes, in concave and convex areas or places of topsoil accumulation conditioned by erosion.…”
mentioning
confidence: 99%