Abstract

The Chaobai River (CBR) basin in northern China is experiencing an unprecedented continuous inflow of external water via the South–North Water Diversion Project, which has channeled water from the southern part of the country to the north. Consequently, the steady rise of groundwater table in recent years is threatening soil salinity regulation. The purpose of this study was to describe the status of salinity of the surface soil in the CBR basin and to evaluate the impact of environmental factors including groundwater table on the spatial distribution of soil salinity using multivariate analysis (MVA) technique. In this study, 10 chemical variables of soil samples collected in 204 sites along CBR were analyzed, considering their interaction with three environmental factors: the density of irrigation canals, groundwater depth and topography. Statistical analysis mainly consisted of principal component analysis (PCA), redundancy analysis (RDA) and clustering analysis (CA). The results allow defining the surface soil in the CBR basin as a slightly saline and moderately alkaline media. The first two axes of multivariate model approximately explains 51% of the observed variability and allows distinguishing two main domains: the saline and the alkaline. The variability of the saline domain, defined by major cations and anions, is obviously controlled by macro environmental factors, of which the density of irrigation canals and groundwater depth contributes 71% and 28%, respectively, while that of the alkaline domain, related to pH and bicarbonate, mainly manifests as singular behaviors of soil groups like rice cultivation or sewage irrigation. The results suggests that more attention should be paid to the ongoing water table rise to help inform future land management decisions and to prevent a double threat of both groundwater and surface water on soil salinization. Meanwhile, this study shows the enormous potential of MVA technique, specifically the complementary duo of RDA and CA, for integrating both global and local information of soil salinity and environmental factors.

Highlights

  • The mother river of the Chinese national capital Beijing and Tianjin municipality—the ChaobaiRiver (CBR), has given birth to generations of civilization and now is the important grain and vegetable base of the two megacities [1,2]

  • The present article reveals the complexity of spatial distribution of the soil salinity in the Chaobai River (CBR) basin, China

  • These soil chemical variables differ depending on the irrigation, groundwater table, terrain, irrigation regulation and the characteristics of the crops

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Summary

Introduction

River (CBR), has given birth to generations of civilization and now is the important grain and vegetable base of the two megacities [1,2]. The CBR basin was once known as a saline–alkaline, waterlogged, flood-prone and low-yielding region due to high groundwater table in the 1950s, and at that time, soil salinity constituted a major factor limiting crop production [3,4] because it affects plant growth and survival [5]. Water 2020, 12, 2104 prevention of the salinization, the area of saline land reducing from 120 to 5 hectares, for which the grain yields increased greatly [6]. The main reason for the reversal of salinization during this period was believed to be related to the increasing demand for water by the society.

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