| 水文与水资源 |
|
|
|
|
| Changes of Runoff and Sediments in Hekou-Longmen Section of the Middle Yellow River |
| WU Rong1,2, CHEN Gao-feng1, ZHANG Jian-xing2 |
| 1.Yangling Vocational & Technical College, Yangling 712100, Shaanxi, China; 2.Key Laboratory for Agricultural Soil and Water Engineering in Arid Area under Ministry of Education, Northwestern Sci-Tech University of Agriculture and Forestry, Yangling 712100, Shaanxi, China |
|
|
|
|
Abstract Soil erosion in Hekou-Longmen section of the middle Yellow river is most serious in China. Recently, the environment of yielding runoff and sediments changed obviously because of implementation of the water conservancy and soil conservation projects on large-scale for many years. Therefore, the study on changing characteristics of runoff and sediments has important significance. The runoff and sediment data of Longmen Hydrological Station during 1957—2005, representing the status of Hehou-Longmen section, were used to analyze the changing characteristics of runoff and sediments by statistical method as Wavelet analysis, Mann-Kendall test, and Difference accumulated curve. The results showed that the variation of runoff and sediments was uneven in the inner-annual distribution and significantly varied in the inter-year distribution. The yearly changes of runoff and sediments all showed decreasing tendency, appeared two or four obviously change periods, respectively. Why? There is good linear relation between the decrease of runoff/sediments and the performance of soil and water conservation measures.
|
|
Received: 09 October 2008
Published: 20 January 2010
|
|
|
[1]陈浩,周金星,陆中臣,等.黄河中游流域环境要素对水沙变异的影响[J].地理研究,2002,21（2）:179-187.
[2]Yang,Z S,Wang H J,Saito,et al.Phase change of the modern Huanghe delta evolution since its last end channel shift in1976 (and its phase change)[C]//5th International Conference of Asian Marine Geology,AGCP2475 DeltaMAP and APN Mega-delta.T.Jarupongsakul,Y.Saito(Ed).Bangkok,Thailand,2004,256.
[3]徐明权,杨小庆.浅谈黄河水沙变化研究成果[J].土壤侵蚀与水土保持学报,1998,14（3）:19-25.
[4]冉大川.黄河中游河龙区间水沙变化研究综述[J].泥沙研究,2000（3）:72-81.
[5]冉大川,上官周平,刘斌,等.河龙区间坝库参数与减沙效益关系研究[J].水土保持学报,2007,21（2）:44-48.
[6]冉大川,罗全华,刘斌,等.黄河中游地区淤地坝减洪减沙及减蚀作用研究[J].水利学报,2004（5）:7-13.
[7]倪晋仁,韩鹏,王光谦,等.黄河中游水保措施对入黄干支流泥沙特性的影响:Ⅱ.减沙效益分析[J].自然资源学报,1997,12（2）:126-132.
[8]穆兴民,巴桑赤烈,ZHANG Lu,等.黄河河口镇至龙门区间来水来沙变化及其对水利水保措施的响应[J].泥沙研究,2007（2）36-41.
[9]徐建华,李雪梅,李世明.河龙区间水利水保工程减沙效益水保法研究成果汇总浅析[J].人民黄河,1995（8）:18-26.
[10]冉大川.黄河中游水土保持措施的减水减沙作用研究[J].资源科学,2006,28（1）:93-100.
[11]尹国康.黄河中游多沙粗沙区水沙变化原因分析[J].地理学报,1998,53（2）:174-183.
[12]魏娜,巩远发,王霄.基于小波变换的陕西夏季降水量变化特征研究[J].中国沙漠,2007,27（6）:1080-1085.
[13]杨建平,丁永建,陈仁升,等.长江黄河源区水文和气象序列周期变化分析[J].中国沙漠,2005,25(3):351-355.
[14]赵燕宁,时兴合,秦宁生.青海南部地区40多年来气候变化的特征分析[J].中国沙漠,2005,25(4):456-462.
[15]Libiseller C,Grimvall A.Performance of Partial Mann-Kendall test for trend detection in the presence of covariates[J].Environmetrics,2002,13:71-84.
[16]马晓波,胡泽勇.青藏高原40年来降水变化趋势及突变的分析[J].中国沙漠,2005,25（1）:137-139.
[17]Bobrovitskaya N N,Kokorev A V,Lemeshko N A.Regional patterns in recent trends in sediment yields of Eurasian and Siberian rivers[J].Global and Planetary Change,2003,39:127-146.
[18]戴仕宝,杨世伦,郜昂,等.近50年来中国主要河流入海泥沙变化[J].泥沙研究,2007（2）:49-58.
[19]蓝永超,丁永建,康尔泗.黑河流域水资源动态变化及其趋势的灰色Markov链预测[J].中国沙漠,2003,23(4):435-440.
[20]蓝永超,丁永建,刘进琪,等.气候变暖情景下黑河山区流域水资源的变化[J].中国沙漠,2005,25(6):863-868.
[21]时兴合,秦宁生,汪青春,等.黄河上游径流变化特征及其影响因素初步分析[J].中国沙漠,2007,27（4）:690-897. |
| No Suggested Reading articles found! |
|
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
| |
Shared |
|
|
|
|
| |
Discussed |
|
|
|
|
2010, Vol. 30 
