马莲河全新世古洪水沉积学和水文学研究

doi:10.11820/dlkxjz.2011.09.002

Abstract

Abstract: Through investigations in the middle and lower reaches of Malian River, Holocene palaeoflood slackwater deposition profile were identified in Heshui County. Samples of the palaeoflood slackwater deposits were collected, and the grain-size distribution and the quartz grain surface texture were examined. All of these indexes showed that the slackwater deposits were typical in the study area. Stratigraphic correlations showed that the slackwater deposits recorded the largest floods occurred between 4200-4000 a B.P. on the river. The flood peak discharges were estimated to be 16780-17200 m³/s by using the slope-area method. Reconstruction of the peak discharge of the 2003 and 2005 floods with the same method and indicators showed that the palaeoflood reconstruction was reliable. These results are important for hydraulic engineering and flood control along the Malian River.

Key words: flood stage indicator, Holocene, Malian River, palaeoflood, slackwater deposits

ZHOU Fang, ZHA Xiaochun, HUANG Chunchang, WANG Xiaqing, SANG Jingjing. Study on Holocene Paleoflood in Malian River Basin[J].PROGRESS IN GEOGRAPHY, 2011, 30(9): 1081-1087.

References

[1] 王英武. 庆阳地区水资源问题及对策. 甘肃农业, 2002(5): 45-46.

[2] 惠俊堂. 马莲河流域“2003.8”暴雨洪水调查分析. 水文,2008, 28(3): 95-96.

[3] 周芳, 查小春, 王夏青. 马莲河流域洪涝灾害及洪水频率分析研究. 江西农业学报, 2010, 22(7): 139-141.

[4] Baker V R. Palaeoflood hydrology in a global context.Catena, 2006, 66(1-2): 161-168.

[5] 詹道江, 谢悦波. 古洪水研究. 北京: 中国水利水电出版社, 2001: 1-83.

[6] Yang D Y, Yu B, Xie Y B, et al. Sedimentary records oflarge Holocene floods from the middle reaches of the YellowRiver, China. Geomorphology, 2000, 33(1-2): 73-88.

[7] Huang C C, Pang J L, Zha X C, et al. Extraodinary floodsof 4100-4000 a B.P. recorded at the late Neolithic Ruinsin the Jinghe river gorges, middle reach of the Yellow river,China. Palaeogeography, Palaeoclimatology, Palaeoecology,2010, 289(1-4): 1-9.

[8] Zha X C, Huang C C, Pang J L. Palaeofloods recorded byslackwater deposits on the Qishuihe River in the MiddleYellow River. Journal of Geographical Sciences, 2009, 19(8): 681-690.

[9] 谢悦波, 杨达源. 古洪水平流沉积基本特征. 河南大学学报, 1998, 26(6): 5-10.

[10] 谢悦波, 王文辉, 王平. 古洪水平流沉积粒度特征. 水文, 2000, 20(4): 18-20.

[11] 谢悦波, 费宇红, 沈起鹏. 古洪水平流沉积与水位. 地球学报, 2001, 22(4): 320-323.

[12] 姚平, 黄春长, 庞奖励, 等. 北洛河中游黄陵洛川段全新世古洪水研究. 地理学报, 2008, 63(11): 1198-1206.

[13] 李瑜琴, 黄春长, 查小春, 等. 泾河中游龙山文化晚期特大洪水水文学研究. 地理学报, 2009, 64(5): 541-552.

[14] 查小春, 黄春长, 庞奖励. 关中西部漆水河全新世特大洪水与环境演变. 地理学报, 2007, 62(3): 292-300.

[15] 贾工作. 马莲河泥沙含量初步分析. 甘肃水利水电技术,2004, 40(4): 365-366.

[16] 贾西安. 加强管护是提高造林保存率的关键. 中国水土保持, 2004(1): 31-32.

[17] 张贵义, 曹家泉, 王治军, 等. 陇东黄土工程地质. 西安:陕西科学技术出版社, 2001: 5-8.

[18] 骆承政. 中国历史大洪水调查资料汇编. 北京: 中国书店, 2006: 164-165.

[19] 任明达, 缪昕. 石英砂表面的微结构: 一种沉积环境标志. 地质论评, 1984, 30(1): 36-41.

[20] 方小敏. 试从兰州地区黄土石英砂表面特征探讨黄土物质来源、成因及环境变迁//中国第四纪冰川与环境研究中心, 中国第四纪研究委员会. 中国西部第四纪冰川与环境. 北京: 科学出版社, 1991: 138-148.

[21] Huang C C, Pang J L, Zhou Q Y, et al. Holocene pedogenicchange and the emergence and decline of rain-fed cerealagriculture on the Chinese Loess Plateau. QuatemaryScience Reviews, 2004, 23(23-24): 2525-2535.

[22] Huang C C, Pang J L, Chen Shu'e. Charcoal records ofthe fire history in the Holocene loess-soil sequences overthe southern Loess Plateau of China. PalaeogeographyPalaeoecology Palaeoclimatology, 2006, 239(1-2): 28-44.

[23]葛本伟, 黄春长, 周亚利, 等. 陇东高原全新世黄土古土壤沉积序列辐射环境研究. 地球与环境, 2009, 37(4):373-380.

[24] 查小春, 黄春长, 庞奖励, 等. 泾河流域不同时间尺度洪水序列频率分析研究. 地理科学, 2009, 29(6): 858-863.

[25] 任明达, 王乃梁. 现代沉积环境概论. 北京: 科学出版社,1981: 8-25.

[26] Vilks G, Wang Y. Surface texture of quartz grains and sedimentaryprocesses on the southeastern Labrador Shelf.Current Research, Part B. Geological Survey of Canada,1981, 18(5): 55-61.

[27] Doornkamp J C, Krinsley D. Electron microscopy appliedto quartz grains from a tropical environment. Sedimentology,1971, 17(1-2): 89-101.

[28] Krinsley D, Doornkamp J C. Atlas of Quart Sand SurfaceTextures. New York: Cambridge University Press,1973: 91.

[29] 王颖, 迪纳瑞尔B. 石英砂表面结构模式图集. 北京: 科学出版社, 1985: 1-10.

[30] 陈丽华, 缪昕, 于众. 扫描电镜在地质上的应用. 北京:科学出版社, 1986: 37-42.

[31] 史辅成, 易元俊, 慕平. 黄河历史洪水调查、考证和研究. 郑州: 黄河水利出版社, 2002: 8-24.

[32] Huang C C, Zhao S C, Pang J L, et al. Climatic aridityand the relocations of the Zhou Culture in the southernLoess Plateau of China. Climatic Change,2003, 61(3):361-378.

[33] 刘东生, 郭正堂, 吴乃琴, 等. 史前黄土高原的自然植被景观: 森林还是草原? 地球学报, 1994, 15(2): 226-234.

[34] 孙爱芝, 冯兆东, 唐领余, 等. 13ka B.P.以来黄土高原西部的植被与环境演化. 地理学报, 2008, 63(3): 280-292.

[35] 李小强, 安芷生, 周杰, 等. 全新世黄土高原塬区植被特征. 海洋地质与第四纪地质, 2003, 23(3): 109-114.

[36] 任美锷. 黄河的输沙量: 过去、现在和将来——距今15万年以来的黄河泥沙收支表. 地球科学进展, 2006, 21(6): 551-563.

[37] 武汉水利电力学院水力学教研室编. 水力学. 北京: 高等教育出版社, 1986: 35-336.

Study on Holocene Paleoflood in Malian River Basin

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