重囗另类BBWSeⅹHD,av狼论坛,精品一卡2卡三卡4卡乱码理论,体育生gv老师浪小辉3p警察

Sediment transferring function of th

時間:2023-04-27 14:48:06 天文地理論文 我要投稿
  • 相關(guān)推薦

Sediment transferring function of the lower reaches of the Yellow River influenced by drainage basin factors and human a

Sediment transferring function (Fs) of rivers is defined and indexed in this study, based on the concept of sediment budget at river reach scales. Then, study is made on the Fs of the lower reaches of the Yellow River in relation to natural and human factors in the drainage basin, such as the annual precipitation in different water and sediment source areas, proportion of >0.05 mm sediment of the total sediment load to the lower reaches of Yellow River, the regulated degree of the "clear" baseflow from the drainage area above Lanzhou, frequency of hyperconcentrated flows, area of soil and water conservation measures in the drainage basin. As a result, a multiple regression equation has been established between Fs and 7 influencing factors, with multiple correlation coefficient r = 0.90.The reduction in annual precipitation in different water and sediment source areas has different effects on Fs. The reduction in annual precipitation in the area above Hekou Town and the area between Longmen and Sanmenxia results in a reduction in Fs, but the reduction in annual precipitation in the area between Hekou Town and Longmen results in an increase in Fs. The grain size composition of sediment load strongly affects the Fs; the larger the proportion of >0.05 mm sediment in the suspended sediment load entering the lower reaches of the Yellow River is, the lower the Fs will be. Thus, if the Xiaolangdi Reservoir traps coarse sediment and releases fine sediment, Fs will be enhanced. This study also shows that the lower the proportion of high-flow season river flow to the annual total river flow at Lanzhou Station is, the lower the Fs will be. Therefore, the interception of large quantities of clear water by the reservoirs on the upper reaches of Yellow River is one of the major causes for the decrease in Fs in the lower reaches of the Yellow River.

作 者: XU Jiongxin   作者單位: Institute of Geographical Sciences and Natural Resources Research, ChineseAcademy of Sciences, Beijing 100101, China  刊 名: 中國科學(xué)D輯(英文版)  SCI 英文刊名: SCIENCE IN CHINA (EARTH SCIENCES)  年,卷(期): 2005 48(12)  分類號: P5  關(guān)鍵詞: river sediment   channel sedimentation   drainage basin factors   human activities   Yellow River  

【Sediment transferring function of th】相關(guān)文章:

TH學(xué)校致高一新生家長的一封信09-29

主站蜘蛛池模板: 青龙| 青阳县| 当雄县| 石柱| 茶陵县| 巴中市| 盐城市| 平定县| 志丹县| 双流县| 永泰县| 古浪县| 申扎县| 蓝山县| 晋中市| 毕节市| 镇平县| 宣武区| 巴东县| 读书| 武鸣县| 西畴县| 兖州市| 迁安市| 海丰县| 嫩江县| 望城县| 惠安县| 昭苏县| 碌曲县| 伊金霍洛旗| 临夏市| 黎川县| 莱西市| 乐至县| 永宁县| 饶平县| 石首市| 永靖县| 恩施市| 怀柔区|