Topographic and Climatic Factors Effect Spatiotemporal Coupling Relationship of Soil Water Conservation Function with Vegetation in Source of the Yellow River

Author:

Zhang Xiaoning1ORCID,Li Xiaodan2,Nian Lili3,Samuel Adingo4,Liu Xingyu3ORCID,Liu Xuelu1,Hui Caihong1ORCID,Zhang Miaomiao2

Affiliation:

1. College of Resources and Environmental Sciences, Gansu Agricultural University, Lanzhou 730070, China

2. College of Management, Gansu Agricultural University, Lanzhou 730070, China

3. College of Forestry, Gansu Agricultural University, Lanzhou 730070, China

4. Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China

Abstract

The Gannan Water Conservation area is an indispensable part of the ecological barrier on the Tibetan Plateau and is a key ecological area for the water supply. Exploring the coupled coordination relationship between vegetation and soil contributes to the conservation and planning of the natural environment. In this study, soil water conservation function (SWCF) was investigated with Moderate Resolution Imaging Spectroradiometer (MODIS) data in the Gannan Water Conservation Area at the source of the Yellow River, and the spatiotemporal coupling relationship between the SWCF and vegetation was explored. Meanwhile, their responses to topographic and climatic factors were investigated with structural equation models. The main results indicated that the coupling coordination degree (DVS) in the soil depth was in a barely coordinated state, with 0–10 cm > 20–30 cm > 10–20 cm, showing that the area proportion of ‘Basic balanced–Synchronous development of VEG and SWCF’ was the highest, and the spatial aggregation feature was obvious. As the gradient of topographic factors varied, the coupling coordination also varied at various soil depths. Meanwhile, the absolute values of the correlation coefficients of the temperature and precipitation with the coupling coordination were the highest at 20–30 cm compared to the other soil depths, demonstrating that the effect was more significant in deeper soils than in shallower ones. Furthermore, the path coefficients of the topographic factors were larger than those of the climatic factors in the 10–20 cm and 20–30 cm layers, while the opposite was true in the 0–10 cm layer. In general, the vegetation conditions and water conservation function of soil in the source area of the Yellow River are basically developing synchronously, and the topographic factor is the key factor for the geographical difference in the coupling relationship between the two factors.

Funder

Scientific Research Start–up Funds

Education Department in Gansu

unified confirmation of right registration of natural resources of Gansu Provincial Land and Resources Department

Publisher

MDPI AG

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