Soil organic carbon distribution in relation to land use and its storage in a small watershed of the Loess Plateau, China

CATENA ◽  
2012 ◽  
Vol 88 (1) ◽  
pp. 6-13 ◽  
Author(s):  
Xuan Fang ◽  
Zhijing Xue ◽  
Bicheng Li ◽  
Shaoshan An
2013 ◽  
Vol 33 (1) ◽  
pp. 179-187 ◽  
Author(s):  
李林海 LI Linhai ◽  
郜二虎 GAO Erhu ◽  
梦梦 MENG Meng ◽  
魏孝荣 WEI Xiaorong

2020 ◽  
Author(s):  
Peng Shi ◽  
Yan Zhang ◽  
Kexin Lu ◽  
Zhaohong Feng ◽  
Yang Yu

<p>Vegetation restoration, terrace and check dam construction are the major measures for soil and water conservation on the Loess Plateau. These effective measures of stabilizing soils have significant impacts on soil organic carbon (SOC) distribution. To understand the impact of land-use changes combined with check dam construction on SOC distribution, 1060 soil samples were collected across a watershed on the Loess Plateau. Forestland, shrubland and terrace had significant higher SOC concentrations in the 0-20 cm soil layer than that of sloping cropland.    Land use change affects the process of runoff and sediment transportation, which has an impact on the migration and transformation of soil carbon. The soil erosion of sloping farmland is the most serious, and the maximum annual erosion rate is as high as 10853.56 t·km<sup>-2</sup>. Carbon sedimented in the dam land was mainly from sloping cropland, and this source percentage was 65%. The application of hydrological controls to hillslopes and along river channels should be considered when assessing carbon sequestration within the soil erosion subsystem. </p>


2018 ◽  
Vol 10 (12) ◽  
pp. 4757 ◽  
Author(s):  
Zhijing Xue ◽  
Shaoshan An

Soil organic carbon (SOC) and total nitrogen (total N) are important soil components for agricultural production. Soil quality is related to the total amount of SOC and total N sequestered in the soil. Land use plays a major role in the distribution and amount of SOC and total N. This study analyses the amount of SOC and total N under various land cover types in 1987, 2005 and 2010, and evaluated their storage in land use conversions in a comprehensively managed watershed on the Loess Plateau, China. Results show that concentrations of SOC and total N in shrub land and natural grassland areas were significantly higher than for other land uses (farmland, orchard, abandoned farmland, manmade grassland) while cropland had the lowest concentration. Storage of SOC and total N increased along the revegetation chronosequence. As the storage of SOC in 2005 and 2010, they were 3461.86 × 108 and 4504.04 × 108 g respectively. Soil organic carbon storage were enhanced one third just during 5 years. The effects of land use on SOC and total N were the most significant in the upper soil layers. The correlation between SOC, total N, and the C/N ratio indicated that the best combination of land uses were natural grassland and shrub land. They efficiently influenced the distribution and storage of SOC and total N, and benefited vegetation restoration.


PLoS ONE ◽  
2014 ◽  
Vol 9 (5) ◽  
pp. e95548 ◽  
Author(s):  
Yaai Dang ◽  
Wei Ren ◽  
Bo Tao ◽  
Guangsheng Chen ◽  
Chaoqun Lu ◽  
...  

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