象山港流域河流形态特征定量分析

doi:10.3969/j.issn.1001-909X.2014.03.007

海洋学研究 ›› 2014, Vol. 32 ›› Issue (3): 50-57.DOI: 10.3969/j.issn.1001-909X.2014.03.007

象山港流域河流形态特征定量分析

袁麒翔^1,2, 李加林^*1,2, 徐谅慧¹, 陈鹏程¹, 王明月¹

1.宁波大学建筑工程与环境学院, 浙江宁波 315211;
2.浙江省海洋文化与经济研究中心,浙江宁波 315211

收稿日期:2014-03-06 修回日期:2014-06-06 出版日期:2014-09-15 发布日期:2022-11-25
通讯作者: *李加林(1973-),男,教授,主要从事海岸带环境与资源开发研究。E-mail:nbnj2001@163.com
作者简介:袁麒翔(1989-),男,浙江舟山市人,主要从事海岸带资源环境方面的研究。E-mail:yqx358@163.com
基金资助:
国家自然科学基金项目资助(41171073,41471004);浙江省自然科学基金项目资助(Y5110321);浙江省哲学社会科学基金项目资助(12JDHY01Z);宁波市社科规划项目资助(G12-XK05);宁波大学优秀学位论文培育基金项目资助(py2013019);浙江省大学生科技创新活动暨新苗人才计划项目资助(2014R405091,2014R405076)

Quantitative analysis of river morphological features in Xiangshan Bay Basin

YUAN Qi-xiang^1,2, LI Jia-lin^*1,2, XU Liang-hui¹, CHEN Peng-cheng¹, WANG Ming-yue¹

1. Faculty of Architectural, Civil Engineering and Environment, Ningbo University, Ningbo 315211, China;
2. Marine Culture and Economic Research Center of Zhejiang Province, Ningbo University, Ningbo 315211, China

Received:2014-03-06 Revised:2014-06-06 Online:2014-09-15 Published:2022-11-25

摘要/Abstract

摘要： 象山港流域发育有自低山流向海洋的众多山溪型河流,形成相对独立的小流域。本文采用流域地貌数学模型与地理信息系统技术相结合的方法,对港湾内小尺度河流特征进行了定量分析。结果表明:(1)象山港流域河流的河长分维值普遍较小,大嵩江的河长最长且主河道最为蜿蜒曲折;(2)凫溪和大嵩江的水系结构较象山港流域其它河流的结构更为复杂且发育更加充分;(3)除了颜公河和钱仓河外,流域内大部分河流纵剖面线呈现下凹型且主河道有多次阶梯状起伏;(4) 基岩性S-A模型的应用具有一定的局限性,凫溪和大嵩江的基岩河床处于均衡状态。

关键词: 小尺度河流, 分维值, 河流纵剖面, 定量分析

Abstract: There are many small-scale mountain rivers in Xiangshan Bay Basin, which flow from low mountains to the sea and form a relatively independent small watershed. In this study, the small-scale river features in the inner bay were quantitatively analyzed by the combined method of fluvial landform mathematical model and geographic information system technology. The results show that: (1)Dasong River is the longest and the most meandering river in Xiangshan Bay Basin, whose river fractal dimension value is generally small. (2)The river structures of Fuxi Stream and Dasong River are more complicated and well-developed than those of other rivers in Xiangshan Bay Basin. (3) Overall, apart from the some rivers (such as Yangong River and Qiancang River), other rivers show a trend of concave and stair-step shape. (4)The applications of S-A model has a certainty limitation. Fuxi Stream and Dasong River's bedrock riverbeds are in equilibrium in the S-A model.

Key words: small-scale rivers, fractal dimension data, river longitudinal profile, quantitative analysis

中图分类号:

P931

袁麒翔, 李加林, 徐谅慧, 陈鹏程, 王明月. 象山港流域河流形态特征定量分析[J]. 海洋学研究, 2014, 32(3): 50-57.

YUAN Qi-xiang, LI Jia-lin, XU Liang-hui, CHEN Peng-cheng, WANG Ming-yue. Quantitative analysis of river morphological features in Xiangshan Bay Basin[J]. Journal of Marine Sciences, 2014, 32(3): 50-57.

参考文献

[1] DONG Zhe-ren. Diversity of river morphology and diversity of bio-communities[J]. Journal of Hydraulic Engineering, 2003,34(11):1-6.
董哲仁.河流形态多样性与生物群落多样性[J].水利学报,2003,34(11):1-6.
[2] CAI Jian-nan,PAN Wei-bin,CAO Ying-zi,et al. Impact of river morphology on urban river self-purification capacity in Guangzhou[J].Water Resources Protection,2010,28(5):16-19.
蔡建楠,潘伟斌,曹英姿,等.广州城市河流形态对河流自净能力的影响[J].水资源保护,2010,28(5):16-19.
[3] YIN Xiao-ling, LI Gui-cai, LIU Kun, et al. Progress on urban stream transformation of critical forms and stability relationships[J]. Progress in Geography,2012,31(7):837-845.
尹小玲,李贵才,刘堃,等.城市河流形态及稳定性演变研究进展[J].地理科学进展,2012,31(7):837-845.
[4] LIANG Hong, LU Juan. The fractal, entropy and geomorphological meaning of Karst drainage[J]. Scientia Geographica Sinica,1997,17(4):310-315.
梁虹,卢娟.喀斯特流域水系分形、熵及其地貌意义[J].地理科学,1997,17(4):310-315.
[5] MANDELBORT B B. The fractal geometry of nature[M]. New York: W.H. Freeman and Company,1983:468.
[6] BARBERA L,ROSSO R.On the fractal dimension of stream networks[J].Water Resources Research,1989,25(4):735-741.
[7] WANG Qian, ZOU Xin-qing, ZHU Da-kui. On the dimensions of Qinhuai river networks based on the GIS technology[J]. Advances in Water Science,2002,13(6):751-756.
王倩,邹欣庆,朱大奎.基于GIS技术的秦淮河流域水系分维研究[J].水科学进展,2002,13(6):751-756.
[8] ZHU Xiao-hua, CAI Yun-long. On box dimensions of river basins of China[J].Advances in Water Science,2003,14(6):731-735.
朱晓华,蔡运龙.中国水系的盒维数及其关系[J].水科学进展,2003,14(6):731-735.
[9] PAN Wei. Study on the morphology of Wei River (Jing River Estuary-Tongguan) based on the fractal geometry,1915-2000A.D[J]. Acta Sedimentologica Sinica,2011,29(5):946-952.
潘威.基于分形理论的1915—2000年渭河泾河口—潼关段河道演变研究[J].沉积学报,2011,29(5):946-952.
[10] CHEN Yan-jie, SONG Guo-cheng, CHEN Zhao-nan. Stream-power incision model for non-steady state orogens[J].Chinese Science Bulletin,2006,51(7):865-869.
陈彦杰,宋国城,陈昭男.非均衡山脉的河流水力侵蚀模型[J].科学通报,2006,51(7):865-869.
[11] ZHANG Hui-ping, ZHANG Pei-zhen, WU Qing-long, et al. Characteristics of The Huanghe River longitudinal profiles around Xunhua-Guide area(Ne Tibet) and their tectonic significance[J]. Quaternary Sciences,2008,28(2):299-309.
张会平,张培震,吴庆龙,等.循化-贵德地区黄河水系河流纵剖面形态特征及其构造意义[J].第四纪研究,2008,28(2):299-309.
[12] ZHAO Hong-zhuang, LI You-li, YANG Jing-chun, et al. The Longitudinal profiles of the ten Rivers in North Tianshan Mountains and their tectonic significance[J]. Acta Geographica Sinica,2009,64(5):563-570.
赵洪壮,李有利,杨景春,等.天山北麓河流纵剖面与基岩侵蚀模型特征分析[J].地理学报,2009,64(5):563-570.
[13] China Bay Records Compiling Committee. Chinese bay records:The fifth section[M]. Beijing: Ocean Press,1992:166-168,193-198.
中国海湾志编纂委员会.中国海湾志-第五分册[M].北京:海洋出版社,1992:166-168,193-198.
[14] HUANG Xiu-Qing, WANG Jin-hui, JIANG Xiao-shan. Marine environment capacity and total pollutant control in Xiangshangang Bay [M].Beijing: Ocean Press,2008:5.
黄秀清,王金辉,蒋晓山.象山港海洋环境容量及污染物总量控制研究[M].北京:海洋出版社,2008:5.
[15] TANG Cong-guo, LIU Cong-qiang. Automated extraction of watershed characteristics based on Arc Hydro Tools: A case study of Wujiang watershed in Guizhou Province, Southwest China[J]. Earth and Environment,2006,34(3):30-37.
唐从国,刘丛强.基于Arc Hydro Tools的流域特征自动提取——以贵州省内乌江流域为例[J].地球与环境,2006,34(3):30-37.
[16] LÜ Ai-feng, CHEN Xi, WANG Gang-sheng. Study on calculation methods of watershed fractal dimention based on DEM[J].Arid Land Geography,2002,25(4):315-320.
吕爱锋,陈嘻,王纲胜.基于DEM的流域水系分维估算方法探讨[J].干旱区地理,2002,25(4):315-320.
[17] CHENG Ji-cheng, JIANG Mei-qiu. Mathematical modelling of morphological processes[M].Beijing: Science Publishing House,1986:34-45,102-108.
承继成,江美球.流域地貌数学模型[M].北京:科学出版社,1986:34-45,102-108.
[18] HE Long-hua, ZHAO Hong. The fractal dimension of river networks and its interpretation[J]. Scientia Geographica Sinica,1996,16(3):124-128.
何隆华,赵宏.水系的分形维数及其含义[J].地理科学,1996,16(3):124-128.
[19] QIAN Ning, ZHANG Ren, ZHOU Zhi-de. Fluvial process theory[M]. Beijing: Science Press,1987:55-66,345.
钱宁,张仁,周志德.河床演变学[M].北京:科学出版社,1987:55-66,345.

象山港流域河流形态特征定量分析

Quantitative analysis of river morphological features in Xiangshan Bay Basin

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 1

编辑推荐

Metrics