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| | The annual average sediment transportation amount was 952. 5 million t and annual averagesediment transportation modulus was 8535 t/km2 in the 1960s in the reaches from Hekouzhen toLongmen of the Yellow River,with an area of 111. 6 thousand km2. Considering the amount retained by reserviors,the actual annual average sediment yield should be 982.4 million t. After deducting slight soil loss area 38.2 million km2 and its annual sediment yield 29. 7 million t,the annual aver... | | 黄河流域河龙区间面积11.16万km2,60年代年均输沙量9.525亿t,年均输沙模数8535t/km2。考虑水库等栏沙,还原计算的年均产沙量为9.824亿t,扣除轻微流失面积3.82万km2及其年产沙量0.297亿t,黄土丘陵沟壑区7.34万km2面积上年均产沙量9、527亿t,年土壤侵蚀摸数为12980t/km2,比年均输沙模数高出52.1%。在小流域泥沙来源分析中,将坡长20m径流小区的年产沙模数改正为自然坡长的年产沙模数,加上坡面浅沟汇流加大冲刷的作用,未治理坡耕地年产沙模数在15000t/km2以上。由此算得的小流域各地类年产沙模数,作为工程规划设计和计算水土保持减沙作用的依据较为接近实际。 | | 文摘来源 | | In the middle reaches of Yellow river basin,a lot of projects have been built.Human activities have changed the land surface and erosion process ,they have also alleviated erosion intensity and retained runoff and sediment. Isograms of sediment transportation modulus and coarse sediment modulus are drawn up based on the obtained data.The variation law of sediment and coarse sediment transportation modulus at areas with more and coarse sedimen... | | 该文根据绘制的黄河中游输沙模数与粗泥沙模数等值线图,研究分析了黄河中游多沙粗沙区输沙模数与粗沙模数变化规律。 | | 文摘来源 | |   |
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