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日照市降雨侵蚀力时空分布特征

杨甲辰 张荣华 齐玉诚 孔凡英 董智

中国水土保持科学2017,Vol.15Issue(5):48-57,10.
中国水土保持科学2017,Vol.15Issue(5):48-57,10.DOI:10.16843/j.sswc.2017.05.007

日照市降雨侵蚀力时空分布特征

Spatial and temporal variations of rainfall erosivity in Rizhao City

杨甲辰 1张荣华 2齐玉诚 1孔凡英 2董智3

作者信息

  • 1. 山东农业大学林学院,山东省土壤侵蚀与生态修复重点实验室/泰山森林生态站,271018,山东泰安
  • 2. 泰安市水土保持生态环境监测站,271000,山东泰安
  • 3. 山东农业大学生命科学学院作物生物学国家重点实验室,271018,山东泰安
  • 折叠

摘要

Abstract

[Background] The Rizhao City,located in the southern coast of Shandong province,is northern rocky mountain soil and the national key harnessing area of Yimeng Mountains and Taishan Mountain,China.However,there are few studies on the soil erosion in the region,and no detailed research on the rainfall erosivity has been carried out specifically for Rizhao City scale.[Methods] In order to investigate the spatial and temporal variations of rainfall erosivity in Rizhao City and improve the scientific nature of soil and water conservation planning and decision-making,we used the daily rainfall data of 61 rainfall stations in Rizhao City from 2005 to 2014 to calculate the rainfall erosivity by the daily rainfall erosivity model,and analyzed the spatial pattern with the help of ArcGIS10 and the temporal variation and the correlation between rainfall,erosive rainfall and rainfall erosivity by virtue of Excel 2013.[Results] 1) For the temporal variability,the annual rainfall erosivity ranged from 1831.55MJmm/(hm2·h·a) to5306.12 MJ·mm/(hm2·h·a),the maximum value(2008) of the average annual rainfall erosivity was 2.90 times of the minimum (2014),and the maximum value (2007) of the rainfall erosivity in flood season was 3.74 times of the minimum (2014).The monthly rainfall erosivity per station was in the range of 1.23 MJ·mm/(hm2 ·h·a) to 1 171.93 MJmm/(hm2 ·h·a),the rainfall erosivity was concentrated from May to September,especially from July to August.2) For the spatial variations,the average rainfall erosivity yearly and in flood season generally increased from inland areas to southeast coastal areas,and the lowest in the central region.Comparing them at the county scale,the highest of the average annual rainfall erosivity was in Lanshan,and then Donggang,the lowest was in Juxian and Wulian.The average annual rainfall erosivity in each station was from 2 755.23 MJ·mm/(hm2·h·a) to 5 061.15 MJmm/(hm2 ·h·a),the average and the median was 3 826.01 MJ·mm/(hm2·h· a) and 3 730.97 MJ· mm/(hm2 · h ·a),respectively,and the standard deviation was 512.81 M J· mm/(hm2· h· a),and the variability coefficients was 13.40%.[Conclusions] The spatial distribution pattern of soil erosion in Rizhao City is not exactly matched with the spatial distribution of rainfall erosivity.In addition to the influence of rainfall erosivity,regional soil erosion is closely related to terrain,soil,vegetation and other factors.To strengthen the research on the comprehensive influence of various factors on soil erosion should be the direction of next step.The results can provide a reference for soil and water conservation planning and decision-making and prediction of soil erosion in Rizhao City.

关键词

降雨侵蚀力/时空分布/日照市/山东省

Key words

rainfall erosivity/spatial and temporal variation/Rizhao City/Shandong Province

分类

农业科技

引用本文复制引用

杨甲辰,张荣华,齐玉诚,孔凡英,董智..日照市降雨侵蚀力时空分布特征[J].中国水土保持科学,2017,15(5):48-57,10.

基金项目

世界银行贷款“山东生态造林生态效益监测与评估”(SEAP-JC-2) (SEAP-JC-2)

欧洲投资银行贷款“山东沿海防护林工程项目”(SCSFP-JC) (SCSFP-JC)

中国水土保持科学

OA北大核心CSCDCSTPCD

1672-3007

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