What is the mass of loess in the Loess Plateau of China?

被引:0
|
作者
Yuanjun Zhu [1 ,2 ,3 ]
Xiaoxu Jia [4 ,3 ]
Jiangbo Qiao [1 ]
Ming'an Shao [1 ,4 ,2 ,3 ]
机构
[1] State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University
[2] College of Resources and Environment, University of Chinese Academy of Sciences
[3] Institute of Soil and Water Conservation, Chinese Academy of Sciences & Ministry of Water Resources
[4] Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences
基金
中国国家自然科学基金;
关键词
The Loess Plateau; Loess mass; Pedotransfer function; Soil erosion; Bulk density;
D O I
暂无
中图分类号
S157.1 [水土流失的原因及其防治];
学科分类号
摘要
The Loess Plateau of China(LP) has the largest and thickest loess deposits in the world. Quantifying the amount of loess in the LP is crucial for investigating the accumulation and erosion of loess, and determining the regional soil and water resource capacity. We used loess thickness data, a pedotransfer function for bulk density(BD), and the clay content data observed in 242 sites across the LP to derive the BD of loess and then estimate the loess mass and its distribution across the LP. The results indicated that the average BD of loess between the surface and bedrock is 1.58 g cm, varying from 1.18 to 1.87 g cm.The total loess mass is approximately 5.45 ? 10t, and the average loess mass over an area of 1 m~2 is 169 t, ranging from 1.36 to 585 t. The greatest mass of loess is in the south-central of the LP while the lowest mass of loess is in the northwest and river valley areas. Our estimate of loess mass provides key data for calculating water, carbon, and nutrient storages in the LP, which improves our understanding of soil-water processes and ecohydrological systems in this landscape.
引用
收藏
页码:534 / 539
页数:6
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