气候变化领域集成服务门户

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(-3), varying from 1.18 to 1.87 g cm(-3). The total loess mass is approximately 5.45 x 10(13) t, 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. (C) 2019 Science China Press. Published by Elsevier B.V. and Science China Press. All rights reserved.