Zhu Yuanjun, Jia Xiaoxu, Qiao Jiangbo, Shao Ming'an
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling 712100, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences & Ministry of Water Resources, Yangling 712100, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100190, China.
Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100190, China.
Sci Bull (Beijing). 2019 Apr 30;64(8):534-539. doi: 10.1016/j.scib.2019.03.021. Epub 2019 Mar 22.
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 × 10 t, and the average loess mass over an area of 1 m 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.
中国黄土高原拥有世界上面积最大、厚度最厚的黄土堆积。量化黄土高原的黄土量对于研究黄土的堆积与侵蚀以及确定区域土壤和水资源容量至关重要。我们利用黄土厚度数据、一个用于容重(BD)的土壤传递函数以及在黄土高原242个地点观测到的黏粒含量数据,推导出黄土的容重,进而估算黄土质量及其在黄土高原的分布。结果表明,地表至基岩之间黄土的平均容重为1.58克/立方厘米,范围在1.18至1.87克/立方厘米之间。黄土总质量约为5.45×10吨,每1平方米面积上的黄土平均质量为169吨,范围在1.36至585吨之间。黄土质量最大的区域位于黄土高原中南部,而黄土质量最小的区域位于西北部和河谷地区。我们对黄土质量的估算为计算黄土高原的水、碳和养分储量提供了关键数据,有助于我们更好地理解该地区的土壤-水过程和生态水文系统。