山东省药乡小流域侵蚀性降雨分布特征

doi:10.16843/j.sswc.2017.01.016

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Abstract [Background] In order to study the effect of erosive rainfall on runoff and sediment yield in the mountainous area of North China, we first need to study the distribution characteristics of erosive rainfall. In this paper, the research object is runoff plot of bare land that is typical in Yaoxiang Small Watershed of Shandong Province. [Methods] The characteristics of erosive rainfall were analyzed by mathematical statistics, based on the data of rainfall observed by tipping bucket rain gauge, runoff calculated by plot runoff and sediment yield measured by oven-drying method in the period of 2013—2015. In addition, rainfall erosive force was calculated by I_30max. In this paper, erosive rainfall standard was proposed by the method of Wang Wanzhong. Here is the method: 1) calculating the total erosion amount of erosive rainfall: the rainfalls of the selected samples are sorted by descending order, and the corresponding amount of soil erosion is accumulated, thus the total erosion amount in n erosive rainfalls is obtained; 2) classifying the amounts of rainfalls as several levels, and then calculating the proportion of the accumulated erosion amount over a given rainfall amount to the total erosion amount; 3) the standard of erosive rainfall is the amount of rainfall corresponding to the proportion of the accumulated soil erosion amount after the allowable soil erosion is deleted, to total erosion amount. [Results] 1) The reference value of standard erosive rainfall in the study area was 17.3 mm. 2) In July, times of erosive rainfall, precipitation, runoff volume, and sediment yield accounted for 42.31%, 45.71%, 85.78%, and 97.97% in all erosive rainfalls, respectively, and erosive rainfall occurred little in other months. 3) In the class of heavy rain, the rainfall times of high rainfall intensity type accounted for 60% and sediment yield accounted for 75.0%. While in the class of above rainstorm, the rainfall times of high rainfall intensity type accounted for 100% and sediment yield accounted for 100%. 4) In the class of rainfall erosive force >1 000 MJ·mm/(h·hm²), sediment yield accounted for 95.26% in all erosive rainfalls, and the runoff depth was over 3 times of the erosive rainfall < 1 000 MJ·mm/(h·hm²). [Conclusions] Therefore, the standard of erosive rainfall in the study area is 17.3 mm, which is mainly distributed in the moderate and above rainfall grades. The rainfall causing serious soil erosion is high rainfall intensity type or the erosive force of the rainfall is > 1 000 MJ·mm/(h·hm²), and it mainly distributes in July. This research is conducive to study the erosive rainfall in the small watershed, and provides a reference for understanding the erosive rainfall in the northern rocky mountains.

Key words： small watershed erosive rainfall erosive rainfall standard rainfall intensity rainfall erosion force

Received: 06 April 2016

PACS:

S157.1

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	Articles by authors
	ZHANG Xinggang
	WANG Chunhong
	CHENG Tiantian
	LI Sai
	LI Yiran
	ZHANG Yongtao

Cite this article:

ZHANG Xinggang,WANG Chunhong,CHENG Tiantian, et al. Distribution characteristics of erosive rainfall in Yaoxiang Small Watershed of Shandong Province[J]. SSWC, 2017, 15(1): 128-133.

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http://journal12.magtechjournal.com/Jweb_stbc/EN/10.16843/j.sswc.2017.01.016 OR http://journal12.magtechjournal.com/Jweb_stbc/EN/Y2017/V15/I1/128

[1]	章文波,谢云,刘宝元.中国降雨侵蚀力空间变化特征[J].山地学报,2003,21(1): 33. ZHANG Wenbo, XIE Yun, LIU Baoyuan. The spatial variation characteristics of rainfall erosion in China[J]. Mounta in Research.2003, 21(1): 33.
[2]	WISCHMEIER W H, SMITH D D. Predicting rainfall erosion losses from cropland east of the Rocky Mountains: a guide for selection of practices for soil and water conservation. AgricHandb 282[M].Washington, DC:USDA ,1965.
[3]	WISCHMEIER W H, SMITH D D. Predicting rainfall erosion losses: a guide to conservation planning. AgricHandb537[M]. Washington, DC:USDA, 1978.
[4]	王万忠.黄土地区降雨特性与土壤流失关系的研究III:关于侵蚀性降雨标准的问题[J].水土保持通报,1984,4(2):58. WANG Wanzhong. Study on the relationship between rainfall characteristics and soil loss in loess area III: [J]. Bulletin of Soil and Water Conservation, 1984, 4, (2): 58.
[5]	谢云,刘宝元.侵蚀性降雨标准研究[J].水土保持学报,2000,12(1):6. XIE Yun, LIU Baoyuan. Study on the standard of erosive rainfall [J]. Journal of Soil and Water Conservation, 2000,12 (1): 6.
[6]	张岩,朱清科.黄土高原侵蚀性降雨特征分析[J].干旱区资源与环境,2006,20(6):99. ZHANG Yan, ZHU Qingke. An analysis of the characteristics of erosive rainfall on the Loess Plateau[J].Journal of Arid Land Resources and Environment ,2006,20(6): 99.
[7]	张文源,王百田,杨光檄,等.喀斯特黄壤区侵蚀性降雨及产沙特征分析[J]. 生态环境学报,2014,23(11):1776. ZHANG Wenyuan, WANG Baitian, YANG Guangxi, et al. Analysis of rainfall erosion and sediment characteristics of Karst yellow soil [J].Ecology and Environment, 2014,23 (11): 1776.
[8]	周大淜,熊明彪,林立金,等. 坡度对紫色土坡耕地侵蚀性降雨值的影响[J]. 水土保持通报,2009,29(6):159. ZHOU Daping, XIONG Mingbiao, LIN Lijin, et al. Influence of rainfall erosion slope value [J]. Bulletin of Soil and Water Conservation, 2009,29(6): 159.
[9]	李林育,王志杰,焦菊英. 紫色丘陵区侵蚀性降雨与降雨侵蚀力特征[J]. 中国水土保持科学,2013,1:8. LI Linyu, WANG Zhijie, JIAO Juying. Characteristics of erosive rainfall and soil erosion in purple hilly region [J].Science of Soil and Water Conservation, 2013, 1:8.
[10]	顾璟冉,张兴奇,顾礼彬,等. 黔西高原侵蚀性降雨特征分析[J]. 水土保持研究,2016,2:39. GU Jingran, ZHANG Xingqi, GU Libin, et al. Analysis of the characteristics of soil and water conservation of the erosive rainfall in the Qianxiplateau[J].Research of Soil and Water Conservation 2016,2:39.
[11]	径流小区和小流域水土保持监测手册[M].北京:中国水利水电出版社, 2015,1:14 Handbook of Soil and Water Conservation Monitoring in Runoff Plot and Small Watershed[M]. Beijing: China Water Conservancy and Hydropower Press, 2015,1:14.
[12]	左长清,马良.天然降雨对红壤坡地侵蚀的影响[J].水土保持学报,2005,19(2):1. ZUO Changqing, MA Liang. Effect of natural rainfall on soil erosion in red soil[J].Journal of Soil and Water Conservation, 2005,19 (2): 1.
[13]	金建君.谢云,张科利.不同样本序列下侵蚀性雨量标准的研究[J].水土保持通报,2001,21(2):31. JIN Jianjun, XIE Yun, ZHANG Keli. Keep the different sample sequence of [J]. Bulletin of Soil and Water Conservation, 2001,21 (2): 31.
[14]	汪邦稳,方少文, 宋月君, 等. 赣北第四纪红壤区侵蚀性降雨强度与雨量标准的确定[J].农业工程学报, 2013, 29(11): 100. WANG Bangwen, FANG Wei, SONG Yuejun, et al. Determination of erosive rainfall intensity and rainfall standard of Quaternary red soil region in the north of Jiangxi Province [J]. Chinese Society of Agricultural Engineering, 2013,29(11): 100.
[15]	王万忠, 焦菊英. 中国的土壤侵蚀因子定量评价研究[J]. 水土保持通报, 1996, 16(5):1. WANG Wanzhong, JIAO Juying. Study on quantitative evaluation of soil erosion factors in China [J]. Bulletin of Soil and Water Conservation, 1996, 16(5): 1.
[16]	刘和平,袁爱萍,路炳军,等.北京侵蚀性降雨标准研究[J].水土保持研究,2007,14(1):215. LIU Heping, YUAN Aiping, LU Bingjun,et al. Study on the standard of erosive rainfall in Beijing. [J]. Science of Soil and Water Conservation, 2007, 14(1): 215.
[17]	蒋荣.地形因子对贵州喀斯特地区坡面土壤侵蚀的影响[D].南京:南京大学,2013. JIANG Rong. Study on effects of topographic factors on soil erosion in Karst area of Guizhou [D]. Nanjing: Nanjing University, 2013.
[18]	侯建才,李占斌,崔灵周. 黄土高原典型流域次降雨径流侵蚀产沙规律研究[J]. 西北农林科技大学学报(自然科学版),2008,36(2):210. HOU Jiancai, LI Zhanbin, CUI Lingzhou. Study on runoff erosion and sediment yield in typical watershed of Loess Plateau [J]. Journal of Northwest Agriculture and Forestry University (Natural Science Edition),2008,36(2):210.