4.6 Article

Long-Term (1990-2013) Changes and Spatial Variations of Cropland Runoff across China

期刊

WATER
卷 14, 期 18, 页码 -

出版社

MDPI
DOI: 10.3390/w14182918

关键词

cropland; runoff estimation; SCS-curve number; spatial interpolation; rainfall; irrigation

资金

  1. Zhejiang Provincial Key Research and Development Program of China [2019C02047]
  2. Zhejiang Provincial Natural Science Foundation of China [LR19D010002]
  3. National Natural Science Foundation of China [41877465, 42107393]
  4. National Key Research and Development Program of China [2021YFD1700802]

向作者/读者索取更多资源

This study quantified the long-term changes and regional spatial variations of cropland runoff in China by combining the Soil Conservation Service Curve Number (SCS-CN) method and geostatistical approaches. The study estimated the national annual cropland runoff volume and runoff depth, and found that rainfall was the main source of cropland runoff for the entire nation. The study also highlighted the need for regionally specific water management strategies to reduce excessive runoff and increase water utilization efficiencies.
Quantitative information on regional cropland runoff is important for sustainable agricultural water quantity and quality management. This study combined the Soil Conservation Service Curve Number (SCS-CN) method and geostatistical approaches to quantify long-term (1990-2013) changes and regional spatial variations of cropland runoff in China. Estimated CN values from 17 cropland study sites across China showed reasonable agreement with default values from the National Engineering Handbook (R-2 = 0.76, n = 17). Among four commonly used geostatistical interpolation methods, the inverse distance weighting (IDW) method achieved the highest accuracy (R-2 = 0.67, n = 209) for prediction of cropland runoff. Using default CN values and the IDW method, estimated national annual cropland runoff volume and runoff depth in 1990-2013 were 253 +/- 25 km(3) yr(-1) and 182 +/- 15 mm yr(-1), respectively. Estimated cropland runoff depth gradually increased from the drier northwest inland region to the wetter southeast coastal region (range: 2-1375 mm yr(-1)). Regionally, eastern, central and southern China accounted for 39% of the cultivated area and 53% of the irrigated land area and contributed to 68% of the national cropland runoff volume. In contrast, northwestern, northern, southwestern and northeastern China accounted for 61% of the cultivated area and 47% of the irrigated land area and contributed to 32% of the runoff volume. Rainfall was the main source (72%) of cropland runoff for the entire nation, while irrigation became the main source of cropland runoff in drier regions (northwestern and southwestern China). Over the 24-year study period, estimated cropland runoff depth showed no significant trends, whereas cropland runoff volume and irrigation-contributed percentages decreased by 7% and 35%, respectively, owing to implementation of water-saving irrigation technologies. To reduce excessive runoff and increase water utilization efficiencies, regionally specific water management strategies should be further promoted. As the first long-term national estimate of cropland runoff in China, this study provides a simple framework for estimating regional cropland runoff depth and volume, providing critical information for guiding developments of management practices to mitigate agricultural nonpoint source pollution, soil erosion and water scarcity.

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