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县域尺度风力侵蚀栅格计算结果落地研究
引用本文:魏文杰1,袁 利2,李文龙1,刘卓昊1,高睿瑜1,张荣华1,毛玉磊3. 县域尺度风力侵蚀栅格计算结果落地研究[J]. 水土保持研究, 2023, 30(4): 42-46,52. DOI: 10.13869/j.cnki.rswc.2023.04.031.
作者姓名:魏文杰1  袁 利2  李文龙1  刘卓昊1  高睿瑜1  张荣华1  毛玉磊3
作者单位:(1.山东泰山森林生态系统国家定位研究站/山东农业大学 林学院, 山东 泰安 271018; 2.淮河水利委员会 淮河流域水土保持监测中心站, 安徽 蚌埠 233001; 3.山东水文水环境科技有限公司, 济南 250014)
基金项目:山东省自然科学基金(ZR2020MD023);
摘    要:[目的]探讨基于栅格侵蚀数据确定风力侵蚀地块的状况,为县域尺度侵蚀计算和水土流失栅格计算结果落地等工作提供参考。[方法]以黄泛平原风沙区河南省兰考县为例,基于耕地风力侵蚀模型,采用栅格计算和软件判断方法,结合野外验证,探讨县域尺度风力侵蚀栅格计算结果落实到地块的状况。[结果](1)栅格计算的兰考县耕地风力侵蚀面积为125.91 km2,涉及1 259 128个栅格,侵蚀模数集中分布在200~400 t/(km2·a)。(2)软件判断法统计的耕地风力侵蚀面积为125.08 km2,涉及2 284个地块,侵蚀模数集中在200~400 t/(km2·a);超过50%流失比例的地块占风力侵蚀地块总数的96%,100%流失比例的地块面积分布在0.000 04~0.6 km2。(3)在面积相对误差上,软件判断法与栅格计算法相对误差为0.66%,城关镇最大,达136.50%,张君墓镇最小,为0.56%;在空间分布上,软件判断法比栅格计算法聚集度指数高、离散程度低,空间分布集中、连续性强。(4...

关 键 词:黄泛平原风沙区  耕地风力侵蚀模型  栅格  地块

Study on the Grid Calculation Results of Wind Erosion at County Scale
WEI Wenjie1,YUAN Li2,LI Wenlong1,LIU Zhuohao1,GAO Ruiyu1,ZHANG Ronghua1,MAO Yulei3. Study on the Grid Calculation Results of Wind Erosion at County Scale[J]. Research of Soil and Water Conservation, 2023, 30(4): 42-46,52. DOI: 10.13869/j.cnki.rswc.2023.04.031.
Authors:WEI Wenjie1  YUAN Li2  LI Wenlong1  LIU Zhuohao1  GAO Ruiyu1  ZHANG Ronghua1  MAO Yulei3
Affiliation:(1.Shandong Taishan Forest Ecosystem National Positioning Research Station/College of Forestry, Shandong Agricultural University, Tai'an, Shandong 271018, China; 2.Huaihe River Basin Soil and Water Conservation Monitoring Center of Huaihe River Water Conservancy Commission, Bengbu, Anhui 233001, China; 3.Shandong Hydrology and Water Environment Technology Co., Ltd., Jinan 250014, China)
Abstract:[Objective] This paper discusses the situation of determining wind eroded land plot based on grid erosion data, providing reference for county scale erosion calculation and soil erosion grid calculation results landing. [Methods] Lankao County, Henan Province, in the Yellow River alluvial area was taken as an example. Based on the wind erosion model of cultivated land, grid calculation and software judgment method combined with field verification were used to explore the implementation of grid calculation results of wind erosion at county scale to plots. [Results](1)The wind erosion area of cultivated land in Lankao County was 125.91 km2, involving 1 259 128 grids, and the erosion modulus concentrated in the range of 200 t/(km2·a)and 400 t/(km2·a).(2)The wind erosion area of cultivated land calculated by software judgment method was 125.08 km2, involving 2 284 plots, and the erosion modulus concentrated between 200 t/(km2·a)and 400 t/(km2·a). The plots with more than 50% in loss proportion accounted for 96% of the total plots eroded by wind, and the plots with 100% in loss proportion ranged from 0.000 04 km2 to 0.6 km2.(3)In terms of area relative error, the relative error of software judgment method and grid calculation method was 0.66%, the relative error for Chengguan Town was the largest(136.50%), and the relative error for Zhangjunmu Town was the smallest(0.56%). In the spatial distribution, the software judgment method had higher aggregation index and lower dispersion degree than the grid calculation method, and the spatial distribution was concentrated and continuous.(4)In the field validation, the intensity of 34 wind-erosion plots was consistent with the software judgment method, with an agreement rate of 68%. [Conclusion] Under the premise of controlling the land area of cultivated land, the software judgment method was feasible and reasonable to implement the results of wind erosion calculated by grid into the land area.
Keywords:Yellow River alluvial area  wind erosion model of cultivated land  grid  plot
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