IMHE OpenIR  > 山地灾害与地表过程重点实验室
137cstracingdynamicsofsoilerosionorganiccarbonandtotalnitrogeninterracedfieldsandforestlandinthemiddlemountainsofnepal
Su Zhengan1; Xiong Donghong1; Deng Wei1; Dong Yifan1; Ma Jing2; Padma C Poudel3; Sher Gurung B3
2016
Source Publicationjournalofmountainscience
ISSN1672-6316
Volume13Issue:10Pages:1829
AbstractThe Middle Mountains is one of the regions of Nepal most vulnerable to water erosion, where fragile geology, steep topography, anomalous climatic conditions, and intensive human activity have resulted in serious soil erosion and enhanced land degradation. Based on the ~(137)Cs tracing method, spatial variations in soil erosion, organic carbon, and total nitrogen(TN) in terraced fields lacking field banks and forestland were determined. Soil samples were collected at approximately 5 m and 20 m intervals along terraced field series and forestland transects respectively. Mean ~(137)Cs inventories of the four soil cores from the reference site was estimated at 574.33 ± 126.22 Bq m~(-2)(1 Bq(i.e., one Becquerel) is equal to 1 disintegration per second(1 dps)). For each terrace, the ~(137)Cs inventory generally increased fromupper to lower slope positions, accompanied by a decrease in the soil erosion rate. Along the entire terraced toposequence, ~(137)Cs data showed that abrupt changes in soil erosion rates could occur between the lower part of the upper terrace and the upper part of the immediate terrace within a small distance. This result indicated that tillage erosion is also a dominant erosion type in the sloping farmland of this area. At the same time, we observed a fluctuant decrease in soil erosion rates for the whole terraced toposequence as well as a net deposition at the toe terrace. Although steep terraces(lacking banks and hedgerows) to some extent could act to limit soil sediment accumulation in catchments, soil erosion in the terraced field was determined to be serious. For forestland, with the exception of serious soil erosion that had taken place at the top of slopes due to concentrated flows from a country road situated above the forestland site, spatialvariation in soil erosion was similar to the "standard" water erosion model. Soil organic carbon(SOC) and TN inventories showed similar spatial patterns to the ~(137)Cs inventory for both toposequences investigated. However, due to the different dominant erosion processes between the two, we found similar patterns between the <0.002 mm soil particle size fraction(clay sized) and ~(137)Cs inventories in terraced fields, while different patterns could be found between ~(137)Cs inventories and the <0.002 mm soil particle size fraction in the forestland site. Such results confirm that ~(137)Cs can successfully trace soil erosion, SOC and soil nitrogen dynamics in steep terraced fields and forestland in the Middle Mountains of Nepal.
Language英语
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/32188
Collection山地灾害与地表过程重点实验室
山区发展研究中心
Affiliation1.中国科学院成都山地灾害与环境研究所
2.四川农业大学
3.Central Department of Geography, University Campus, Tribhuvan University
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
Su Zhengan,Xiong Donghong,Deng Wei,et al. 137cstracingdynamicsofsoilerosionorganiccarbonandtotalnitrogeninterracedfieldsandforestlandinthemiddlemountainsofnepal[J]. journalofmountainscience,2016,13(10):1829.
APA Su Zhengan.,Xiong Donghong.,Deng Wei.,Dong Yifan.,Ma Jing.,...&Sher Gurung B.(2016).137cstracingdynamicsofsoilerosionorganiccarbonandtotalnitrogeninterracedfieldsandforestlandinthemiddlemountainsofnepal.journalofmountainscience,13(10),1829.
MLA Su Zhengan,et al."137cstracingdynamicsofsoilerosionorganiccarbonandtotalnitrogeninterracedfieldsandforestlandinthemiddlemountainsofnepal".journalofmountainscience 13.10(2016):1829.
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