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HYDROLOGICAL EFFECT OF URBANIZATION IN YITONG RIVER BASIN

机译:伊龙河流域城市化的水文效应

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Urbanization is a process of land use change dominated by human beings.The rapid urbanization process has changed the underlying surface conditions and affected the hydrological cycle process of the underlying surface of the basin.Based on the analysis of a long series of hydrological data over the past 35 years,combined with the underlying surface data of satellite images in this area,the hydrological effect caused by rapid urbanization in Yitong River Basin is analyzed.The results show that during the period of 1980-2015,the proportion of unused land represented by wetlands and bare sands decreased from 3.84% to 0.48%,cultivated land decreased from 71.34% to 67.9%,and forest land decreased by 14.9% to 11.7%.Urban land increased from 6.75% to 15.25%,and grassland increased from 0.5% to 1.03.Through the SWAT t model we explore influence of change in the underlying surface on the runoff.The results show that the runoff changes are significant from 1980 to 2000,while the runoff changes from 2000 to 2015 are not obvious.The change of the underlying surface reflects the urbanization of the basin in different periods.and the impact on runoff.
机译:城市化是一种被人类主导的土地利用变化的过程。快速的城市化进程改变了潜在的表面条件,并影响了盆地下面的水文循环过程。基于对底部的水文数据的分析在过去的35年里,与卫星图像的潜在表面数据相结合在该地区,分​​析了尤东河流域快速城市化引起的水文效应。结果表明,在1980 - 2015年期间,未使用土地的比例湿地和裸砂从3.84%下降至0.48%,耕地从71.34%下降至67.9%,林地下降14.9%至11.7%.urban土地从6.75%增加到15.25%,草地增加到0.5% 1.03.THROUGHTHROUGH TWAT T模型,我们探讨了潜在地面变化对径流的影响。结果表明,径流变化从1980年到2000年,径流发生变化2000年至2015年的ROM不明显。底层表面的变化反映了盆地在不同时期的城市化。对径流的影响。

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