1. 南京大学 地理与海洋科学学院,江苏,南京,210023
2. 贵州省水土保持监测站,贵州,贵阳,550002
纸质出版:2016
移动端阅览
顾璟冉, 张兴奇, 顾礼彬, 等. 黔西高原地区降雨侵蚀力的简易算法[J]. 水土保持通报, 2016,36(2):204-208.
GU Jingran, ZHANG Xingqi, GU Libin, et al. Simple Algorithm of Rainfall Erosivity in West Guizhou Plateau Area[J]. Bulletin of Soiland Water Conservation, 2016, 36(2): 204-208.
顾璟冉, 张兴奇, 顾礼彬, 等. 黔西高原地区降雨侵蚀力的简易算法[J]. 水土保持通报, 2016,36(2):204-208. DOI: 10.13961/j.cnki.stbctb.2016.02.039.
GU Jingran, ZHANG Xingqi, GU Libin, et al. Simple Algorithm of Rainfall Erosivity in West Guizhou Plateau Area[J]. Bulletin of Soiland Water Conservation, 2016, 36(2): 204-208. DOI: 10.13961/j.cnki.stbctb.2016.02.039.
[目的
]
对黔西高原地区侵蚀性降雨特性进行分析并探索降雨侵蚀力的简易算法
为该区土壤侵蚀预报模型的建立提供理论依据。[方法
]
利用径流小区观测法
基于毕节小区2012-2014年53次降雨过程资料进行分析。[结果
]
(1) 降雨量(P)和最大60 min降雨动能(E
60
)是影响坡面产流、产沙的两个主要因子。坡面产流、产沙与最大60 min雨强(I
60
)显著相关;(2) 坡面产流产沙与二元复合因子的相关系数显示
EI
60
PI
60
和I
30
I
60
是影响坡面产流、产沙的3类主要降雨复合指标
EI
30
和EI
60
与坡面产流产沙的相关系数间相差较小;(3) 基于坡面产流、产沙与降雨单指标和降雨复合指标的相关关系
确定了简易算法的参数。[结论
]
基于可比性
以R=EI
30
作为参照值对3种简易算法的结果进行决定系数和偏差率比较后
得到研究区便捷、快速的降雨侵蚀力简易算法为:R=0.344(PI
60
)。
[Objective] The characteristics of rainfall were analyzed and the simple algorithm of rainfall erosi-vity of West Guizhou plateau area were studied to provide theoretical basis for the building of the soil erosion prediction model. [Methods] 53 rainfall events of Bijie area from 2012 to 2014 were obtained by means of runoff plots observation. [Results] The results showed that: (1) rainfall amount(P) and rainfall energy of 60 minutes(E60) were two important affecting factors on the processes of slope runoff and sediment. Slope runoff and sediment yield were found significantly correlated with rainfall intensity of 60 minutes(I60). (2) The correlation coefficients between runoff/sediment and the mixed factors of rainfall indicated that EI60
PI60 and I30 I60 were three kinds of the most important impacting factors on soil erosion process. What is more
the correlation coefficient between runoff/sediment and EI60 was slightly different with the one between runoff/sediment and EI30. (3) Parameters of simple algorithm of rainfall erosivity were determined based on the above analyses. [Conclusion] Through the comparison of determination coefficients and the average error rates obtained from three algorithms
the simple algorithm of rainfall erosivity of the study area was expressed as R=0.344(PI60) with reference to R=EI30 for its comparability.
Wischmeier W H, Smith D D. Predicting Rainfall Erosion Losses:A Guide to Conservation Planning[J]. US Washington D C:Agriculture Handbook No 537, 1978.
Richardson C W, Foster G R, Wright D A. Estimation of erosion index from daily rainfall amount[J]. Transactions of the ASAE, 1983,26(1):153-156.
章文波,谢云,刘宝元.用雨量和雨强计算次降雨侵蚀力[J].地理研究,2002,21(3):384-390.
严毅,陈登.贵州省毕节市土地石漠化现状与治理对策[J].内蒙古林业调查设计,2011,34(5):43-46.
李瑞,李勇,刘云芳.贵州喀斯特地区降雨与坡面土壤侵蚀关系研究[J].水土保持研究,2012,19(3):3560-3562.
戴海伦,苑爽,张科利,等.贵州省降雨侵蚀力时空变化特征研究[J].水土保持研究,2013,20(1):37-41.
许月卿,周巧富,李双成.贵州省降雨侵蚀力时空分布规律分析[J].水土保持通报,2005,25(4):11-14.
刘斌涛,陶和平,宋春风,等.我国西南山区降雨侵蚀力时空变化趋势研究[J].地球科学进展,2012,27(5):499-509.
罗宁,许炳南,文继芬,等.贵州大气降水的时空分布规律研究[J].贵州气象,2006,30(4):3-7.
王万中,焦菊英,郝小品,等.中国降雨侵蚀力
R
值的计算与分布[J].水土保持学报,1995,9(4):5-18.
伍育鹏,谢云.国内外降雨侵蚀力简易计算方法的比较[J].水土保持学报,2001,15(3):31-34.
王万忠,焦菊英.黄土高原降雨侵蚀产沙与黄河输沙[M].北京:科学出版社,1996.
姚治君,廖俊国,陈传友.云南玉龙山东南坡降雨因子与土壤流失关系的研究[J].自然资源学报,1991,6(1):45-54.
徐丽,谢云,符素华,等.北京地区降雨侵蚀力简易计算方法研究[J].水土保持研究,2007,14(6):433-437.
符素华,段淑怀,吴敬东,等.北京山区次降雨侵蚀力[J].水土保持学报,2002,16(1):37-39.
蒋荣.地形因子对贵州喀斯特地区坡面土壤侵蚀的影响[D].江苏 南京:南京大学,2013.
0
浏览量
1072
下载量
7
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621