Recognition of the Interaction Mechanisms between Water and Land Resources Based on an Improved Distributed Hydrological Model

Author:

Wang Jianwei1ORCID,Lv Xizhi1,Qin Tianling2ORCID,Ni Yongxin13,Ma Li1,Zhang Qiufen1,Nie Hanjiang45ORCID,Lv Zhenyu6,Li Chenhao78ORCID,Zhang Xin2,Feng Jianming9

Affiliation:

1. Yellow River Institute of Hydraulic Research, Henan Key Laboratory of Yellow Basin Ecological Protection and Restoration, Zhengzhou 450003, China

2. State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China

3. College of Hydrology and Water Recourses, Hohai University, Nanjing 210098, China

4. Key Laboratory for Geographical Process Analysis & Simulation of Hubei Province, Wuhan 430079, China

5. School of Urban and Environmental Sciences, Central China Normal University, Wuhan 430079, China

6. China Three Gorges Corporation, Wuhan 430010, China

7. Beijing Laboratory of Water Resources Security, Capital Normal University, Beijing 100048, China

8. Beijing Institute of Hydrogeology, College of Resource Environment and Tourism, Capital Normal University, Beijing 100048, China

9. School of Water Conservancy and Civil Engineering, Zhengzhou University, Zhengzhou 450001, China

Abstract

Conflicts between humans and land use in the process of using water and conflicts between humans and water resources in the process of using land have led to an imbalance between natural ecosystems and socio-economic systems. It is difficult to understand the impact of the processes of water production and consumption on land patches and their ecological effects. A grid-type, basin-distributed hydrological model was established in this study, which was based on land-use units and coupled with groundwater modules to simulate the water production and consumption processes in different units. By combining land use and net primary productivity, the runoff coefficient and the water use efficiency (NPP/ET) of different land units were used as indicators to characterize the interaction between water and land resources. The results showed that the average runoff coefficients of cultivated land, forest land and grassland were 0.7, 0.5 and 0.9, respectively. Moreover, the average runoff coefficients of hills, plains and basins were 0.7, 0.7 and 0.8, respectively. The NPP produced by the average unit, evapotranspiration, in cultivated land, forest land and grassland was 7 (gC/(m2•a))/mm, 0.7 (gC/(m2•a))/mm and 0.2 (gC/(m2•a))/mm, respectively. These results provide quantitative scientific and technological support in favor of the comprehensive ecological management of river basins.

Funder

Excellent Youth Foundation of Henan Scientific Committee

National Natural Sciences Foundation of China

Central Nonprofit Research Institutions Basic Scientific Research Special Fund

Youth Talent Support Program of Zhongyuan

Publisher

MDPI AG

Subject

Water Science and Technology,Aquatic Science,Geography, Planning and Development,Biochemistry

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