1. 陕西师范大学旅游与环境学院,陕西,西安,710062
2. 中国科学院地球环境研究所黄土与第四纪地质国家重点实验室,陕西,西安,710075
纸质出版:2015
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周岳, 赵景波, 穆珍珍. 西安市东郊渭河河漫滩沉积与洪水变化[J]. 水土保持通报, 2015,35(1):73-78.
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.
周岳, 赵景波, 穆珍珍. 西安市东郊渭河河漫滩沉积与洪水变化[J]. 水土保持通报, 2015,35(1):73-78. DOI: 10.13961/j.cnki.stbctb.2015.01.014.
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.
[目的] 通过揭示历史时期洪水的演变
科学地预测洪水的发生
以求减少洪水灾害造成的损失。[方法] 通过分析西安市东郊水流村剖面106个样品的粒度组成
研究了西安市渭河近230 a来的洪水事件。[结果] 剖面厚度约5 m
沉积物主要由粗粉砂、极细砂、中砂和粗砂组成
在各层中变化明显
能够指示古洪水的变化。粒度成分和粒度参数指示
研究剖面中的洪水沉积可分为21层
表明西安市渭河近230 a来至少发生了21次洪水事件
各阶段的洪水动力大小为:第18阶段 >17阶段 >15阶段 >16
19阶段 >21阶段 >4
5阶段 >3阶段 >1
2阶段 >6
7阶段 >10阶段 >11阶段 >8
9阶段 >13
14阶段 >12阶段 >20阶段。在研究剖面发生的21次洪水事件中
除第20次洪水外
其余洪水发生时河漫滩上的洪水深度均大于2 m
均为大洪水事件。[结论] 洪水沉积层的分布和粒度成分指示
第3
5
7
8次大洪水的发生是由于当年降水量的显著增加造成的
其余次洪水的发生可能是当年降水量增加造成的
也可能是当年降水量没有增加而是由于当年降水量集中造成的。
[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.
朱诚.长江三峡库区中坝遗址地层古洪水沉积判别研究[J].科学通报,2005,50(20):2240-2250.
葛兆帅.晚更新世晚期以来的长江上游古洪水记录[J].第四纪研究,2004,24(5):555-560.
Grossman M J. Large floods and climatic change during the Holocene on the Ara River, Central Japan[J]. Geomorphology, 2001,39(1):21-37.
朱向峰,黄春长,庞奖励,等.渭河天水峡谷全新世特大洪水水文学研究[J].地理科学进展,2010,29(7):840-846.
庞雷,陈文军.渭河"2003·8"洪水分析[J].水资源研究,2004,25(4):25-28.
刘小丰,潘保田,高红山,等.渭河L
9
(0.87-0.94 Ma)时期古洪水事件的特征研究[J].干旱区地理,2007,30(2):247-250.
毛明策,王琦.渭河流域近40 a来汛期降水特征分析[J].人民黄河,2010,32(12):64-65.
杨明楠,朱亮.陕西渭河流域水资源开发利用及问题分析[J].地下水,2010,32(6):170-172.
甘枝茂,桑广书,甘锐,等.晚全新世渭河西安段河道变迁与土壤侵蚀[J].水土保持学报,2002,16(2):129-132.
牛俊杰,赵景波,马莉,等.西安北郊渭河河漫滩沉积与洪水事件[J].地理研究,2010,29(8):1484-1492.
赵景波,龙腾文,陈颖.渭河关中段近400 a来洪涝灾害变化研究[J].水土保持通报,2010,30(2):5-8.
赵景波,郁耀闯,周旗.渭河渭南段高漫沉积记录的洪水研究[J].地质评论,2009,55(2):231-241.
史兴民,万正耀.渭河咸阳段近代洪水沉积物力度特征分析[J].水土保持通报,2008,28(3):71-76.
周晓红,赵景波.近120年来高陵渭河河漫滩沉积物磁化率指示的气候变化[J].水土保持学报,2007,21(3):196-200.
阴雷鹏,肖攀,赵景波,等.渭河距今70 a以来洪水演变研究[J].安徽农业科学,2010,28(32):11995-11997,12035.
Giancarlo G B, Nicholas M I. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland[J]. Nature, 1999,397(6719):515-517.
于英文,胡自治,徐长林,等.东祁连山高寒灌丛植被类型与分布特征[J].甘肃农业大学学报,1999,34(1):12-17.
西安市地方志编纂委员会.西安市志:第2卷[M].西安:西安地图出版社,2000:382-388.
谢又予.沉积地貌分析[M].北京:海洋出版社,2000:3-4.
黄思静.用Excel计算沉积物粒度分布参数[J].成都理工学院学报,1999,26(2):196-198.
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