Abstract

Inter-basin water transfer projects are designed to relieve water scarcity around the world. However, ecological problems relating to reductions in protection zone functions can occur during inter-basin transfers. This paper uses the largest inter-basin water transfer project in the world, namely, the South-to-North Water Transfer Project (SNWTP) in China, as an example to analyze the variation of Miyun Reservoir’s inner protection zone functions when water is transferred. Specifically, a riparian model (RIPAM) coupled with remote sensing data were used to calculate the nitrogen (N) and phosphorus (P) losses due to plant uptake, and these results were validated by in situ survey data. Then, correlations between water levels and N and P removal were analyzed. The results show that water table disturbances resulting from elevated water levels strongly influence the growth of plants and have obvious negative impacts on N and P removal in the inner protection zone. With the implementation of the middle route of the SNWTP, the water level of Miyun will rise to 150 m in 2020, and subsequently, the total net primary productivity (NPP) could decline by more than 40.90% from the level in 2015, while the N and P uptake could decline by more than 53.03% and 43.49%, respectively, from the levels in 2015, according to the modeling results. This will lead to declines in the inner protection zone’s defense effectiveness for N and P interception and increases in risks to the security of water resources. The results of this study provide useful knowledge for managing the defense function of the terminal reservoir’s inner protection zone and for ensuring that water quality is maintained during the diversion process.

Highlights

  • Inter-basin water transfers can relieve water scarcity and are a popular water-resource topic.To date, many famous projects have been built to alleviate uneven water resource distributions, such as the Central Arizona Project, the Colorado River Projects and California North-to-South Water TransferProject in the United States [1,2], the Siberian Rivers Diversion in Russia [3], the Snowy MountainsScheme in Australia [4], the National River Linking Project in India [5], and the South-to-North WaterTransfer Project (SNWTP) in China [6]

  • More attention should be devoted to the problems faced in receiving areas of inter-basin water projects because artificial projects can raise the water level of a receiving area and flood its drinking water protection zones, which may result in a decline of surface water quality

  • The total net primary productivity (NPP) will likely be less than the amount of 8454.96 t detected in 1999 when the water level was 149 m, and it is predicted to decline by more than 40.90% compared to the level in 2015

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Summary

Introduction

Inter-basin water transfers can relieve water scarcity and are a popular water-resource topic.To date, many famous projects have been built to alleviate uneven water resource distributions, such as the Central Arizona Project, the Colorado River Projects and California North-to-South Water TransferProject in the United States [1,2], the Siberian Rivers Diversion in Russia [3], the Snowy MountainsScheme in Australia [4], the National River Linking Project in India [5], and the South-to-North WaterTransfer Project (SNWTP) in China [6]. Many famous projects have been built to alleviate uneven water resource distributions, such as the Central Arizona Project, the Colorado River Projects and California North-to-South Water Transfer. Scheme in Australia [4], the National River Linking Project in India [5], and the South-to-North Water. The environmental responses to inter-basin water transfers should be studied. Numerous ecological changes during inter-basin water transfers have been proposed, including the introduction of nonindigenous species, secondary salinization, disturbances in water chemistry and quality, changes in hydrologic regimes, and alterations of habitats [8,11,12,13,14,15,16,17,18]. More attention should be devoted to the problems faced in receiving areas of inter-basin water projects because artificial projects can raise the water level of a receiving area and flood its drinking water protection zones, which may result in a decline of surface water quality

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