ZHOU Yue, ZHAO Jingbo, MU Zhenzhen. Sediment of Floodplain and Flood Change of Weihe River in Eastern Suburb of Xi'an City[J]. Bulletin of Soiland Water Conservation, 2015, 35(1): 73-78.
DOI:
ZHOU Yue, ZHAO Jingbo, MU Zhenzhen. Sediment of Floodplain and Flood Change of Weihe River in Eastern Suburb of Xi'an City[J]. Bulletin of Soiland Water Conservation, 2015, 35(1): 73-78. DOI: 10.13961/j.cnki.stbctb.2015.01.014.
Sediment of Floodplain and Flood Change of Weihe River in Eastern Suburb of Xi'an City
[Objective] To reveal characteristics of the flood events occurred in historical period
scientifically predict the occurrence of flood and reduce the loss caused by flood disasters.[Methods] According to the analysis of grain size for 106 samples from the floodplain deposition of Shuiliu village in the northern suburbs of Xi'an City
the flood events of Weihe river in Xi'an City over the past 230 years was studied.[Results] The section studied was 5 m in thickness and consisted of silt particles
clay sand
middle size sand and coarse sand
which changed distinctly in the stratigraphic section and indicated the flood events very well. Particle size and particle parameters indicated that 21 deposit layers can be determined and at least 21 stages of floods in the section studied in past 230 years. The flood scale of these 21 flood phases were:18 th >17 th >15 th >16 th
19 th >21 th >4 th
5 th >3 rd >1 st
2 nd >6 th
7 th >10 th >11 th >8 th
9 th >13 th
14 th >12 th >20 th. The flood level over the sediment of the floodplain was bigger than 2 m when these 21 flood stages occurred except the 20 th.[Conclusion] The distribution and grain size of flood deposit layers indicated that the occurring reason for the major flood of 3 rd
5 th
7 th and 8 th flood was due to the increase in annual mean precipitation
the rest flood events were due to the increase in annual mean precipitation or concentrated precipitation in a year.