FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2612149097> ?p ?o ?g. }

• W2612149097 endingPage "400" @default.
• W2612149097 startingPage "393" @default.
• W2612149097 abstract "The soils of the Loess Plateau of China exhibit zonal characteristics, with declining clay percentages from the southern to northern regions. However, these differences have been largely ignored in studies of soil erosion and the related organic carbon (OC) loss. The goal of this study was to investigate the effect of gradual changes in soil texture on the loss and selective transport of soil and soil organic carbon (SOC) on the Loess Plateau of China. Four typical soils with decreasing clay contents (26.3%, 21.2%, 15.6% and 12.1%) in Shaanxi Province were selected and studied. Rainfall-simulated experiments were performed in 1 m (width) × 5 m (length) plots with a rainfall intensity of 120 mm h− 1 on three slope gradients (15°, 20° and 25°). The runoff and sediment yields, particle size distributions of the sediments, OC concentrations and enrichment ratios of OC in sediment (ERoc) during rainfall processes were measured and calculated. A comparison of the rainfall characteristics between rainfall events in different soils indicated that a decrease in the clay percentage increased the intensity of rill erosion. The runoff rates of different events decreased with the clay percentage, whereas no general pattern was observed in the sediment yield rate due to differences in the initial timing and intensity of rill erosion. Furthermore, the ERoc values in the sediments of all the events were between 0.64 and 1.44, with 90% of values between 0.80 and 1.20. Similarly, the effective particle size distribution of the sediments exhibited relatively constant values with rainfall duration. Non-significant correlations (P > 0.05) between ERoc and dispersed and non-dispersed sediment particles suggested that the transport of sediment and OC was non-selective. Moreover, significant linear correlations were observed between the amount of SOC loss and sediments in all the events. However, there was no significant difference in total SOC loss between the rainfall events, except for in events with a soil clay percentage of 15.6%. SOC losses in soils with 26.3% and 21.2% clay percentages were mainly due to the high SOC concentrations of the original soils, whereas those in other soils were due to the large amount of lost sediment. However, the variations in soil loss and SOC loss were not associated with changes in the clay content of the soil. These results suggest that zonal soils with decreasing clay contents do not influence the selective transport of OC, but soil textures affect the sediment and SOC loss through complicated mechanisms." @default.
• W2612149097 created "2017-05-19" @default.
• W2612149097 creator A5011250891 @default.
• W2612149097 creator A5031043803 @default.
• W2612149097 creator A5033508386 @default.
• W2612149097 creator A5040647242 @default.
• W2612149097 creator A5043129687 @default.
• W2612149097 creator A5074591122 @default.
• W2612149097 creator A5084407437 @default.
• W2612149097 date "2017-09-01" @default.
• W2612149097 modified "2023-09-27" @default.
• W2612149097 title "Zonal characteristics of sediment-bound organic carbon loss during water erosion: A case study of four typical loess soils in Shaanxi Province" @default.
• W2612149097 cites W1522959645 @default.
• W2612149097 cites W191959266 @default.
• W2612149097 cites W1977159749 @default.
• W2612149097 cites W1981310943 @default.
• W2612149097 cites W1984340520 @default.
• W2612149097 cites W1986465273 @default.
• W2612149097 cites W1987044514 @default.
• W2612149097 cites W1987853641 @default.
• W2612149097 cites W1995214430 @default.
• W2612149097 cites W1996421025 @default.
• W2612149097 cites W1996928068 @default.
• W2612149097 cites W2002049746 @default.
• W2612149097 cites W2007356792 @default.
• W2612149097 cites W2022799505 @default.
• W2612149097 cites W2027319535 @default.
• W2612149097 cites W2033881322 @default.
• W2612149097 cites W2039333532 @default.
• W2612149097 cites W2044930091 @default.
• W2612149097 cites W2045002628 @default.
• W2612149097 cites W2053043516 @default.
• W2612149097 cites W2053978646 @default.
• W2612149097 cites W2056535779 @default.
• W2612149097 cites W2060615563 @default.
• W2612149097 cites W2063995564 @default.
• W2612149097 cites W2067840721 @default.
• W2612149097 cites W2069244422 @default.
• W2612149097 cites W2079359991 @default.
• W2612149097 cites W2087462515 @default.
• W2612149097 cites W2091160252 @default.
• W2612149097 cites W2091221889 @default.
• W2612149097 cites W2093092546 @default.
• W2612149097 cites W2098245583 @default.
• W2612149097 cites W2098908385 @default.
• W2612149097 cites W2110854629 @default.
• W2612149097 cites W2111718697 @default.
• W2612149097 cites W2115009060 @default.
• W2612149097 cites W2144189317 @default.
• W2612149097 cites W2147377505 @default.
• W2612149097 cites W2157462758 @default.
• W2612149097 cites W2166768651 @default.
• W2612149097 cites W2326373345 @default.
• W2612149097 cites W2500246397 @default.
• W2612149097 cites W2511658845 @default.
• W2612149097 cites W2529756480 @default.
• W2612149097 cites W402509215 @default.
• W2612149097 cites W44923620 @default.
• W2612149097 doi "https://doi.org/10.1016/j.catena.2017.05.001" @default.
• W2612149097 hasPublicationYear "2017" @default.
• W2612149097 type Work @default.
• W2612149097 sameAs 2612149097 @default.
• W2612149097 citedByCount "15" @default.
• W2612149097 countsByYear W26121490972017 @default.
• W2612149097 countsByYear W26121490972018 @default.
• W2612149097 countsByYear W26121490972019 @default.
• W2612149097 countsByYear W26121490972020 @default.
• W2612149097 countsByYear W26121490972021 @default.
• W2612149097 countsByYear W26121490972022 @default.
• W2612149097 countsByYear W26121490972023 @default.
• W2612149097 crossrefType "journal-article" @default.
• W2612149097 hasAuthorship W2612149097A5011250891 @default.
• W2612149097 hasAuthorship W2612149097A5031043803 @default.
• W2612149097 hasAuthorship W2612149097A5033508386 @default.
• W2612149097 hasAuthorship W2612149097A5040647242 @default.
• W2612149097 hasAuthorship W2612149097A5043129687 @default.
• W2612149097 hasAuthorship W2612149097A5074591122 @default.
• W2612149097 hasAuthorship W2612149097A5084407437 @default.
• W2612149097 hasConcept C107872376 @default.
• W2612149097 hasConcept C114793014 @default.
• W2612149097 hasConcept C123157820 @default.
• W2612149097 hasConcept C127313418 @default.
• W2612149097 hasConcept C158787203 @default.
• W2612149097 hasConcept C159390177 @default.
• W2612149097 hasConcept C159750122 @default.
• W2612149097 hasConcept C175963888 @default.
• W2612149097 hasConcept C185515318 @default.
• W2612149097 hasConcept C185592680 @default.
• W2612149097 hasConcept C187320778 @default.
• W2612149097 hasConcept C18903297 @default.
• W2612149097 hasConcept C2779135002 @default.
• W2612149097 hasConcept C2816523 @default.
• W2612149097 hasConcept C2993008072 @default.
• W2612149097 hasConcept C39432304 @default.
• W2612149097 hasConcept C39464130 @default.
• W2612149097 hasConcept C50477045 @default.
• W2612149097 hasConcept C76886044 @default.
• W2612149097 hasConcept C86803240 @default.

• next