珠江三角洲千年尺度演变的动态平衡及其唯象判据探讨

吴超羽

doi:10.3969/j.issn.0253-4193.2018.07.002

珠江三角洲千年尺度演变的动态平衡及其唯象判据探讨

doi: 10.3969/j.issn.0253-4193.2018.07.002

吴超羽

中山大学近岸海洋科学与技术研究中心, 广东广州 510275

计量
- 文章访问数: 670
- HTML全文浏览量: 43
- PDF下载量: 242
- 被引次数: 0
出版历程
- 收稿日期: 2018-05-30
- 修回日期: 2018-06-15

A preliminary study on the phenomenological relation between morphodynamic equilibrium and geomorphic information entropy in the evolution of the Zhujiang River Delta

Wu Chaoyu

Center for Coastal Ocean Science and Technology Research, Sun Yat-sen University, Guangzhou 510275, China

摘要

摘要: 本文从学科交叉需要审视"平衡态"这一重要的基本概念在若干学科，包括河口海岸学的异同，简述6 000~2 500 a BP珠江河口三角洲主要动力沉积结构演变。在形态动力模型PRD-LTMM基础上选取水深-面积作为系统表征变量，分析不同子系统的统计特性并构建各自的信源概率空间，计算子系统水深信息熵的时间序列。通过比较沉积动力结构演变和地貌信息熵序列，发现地貌信息熵可以作为在给定意义上的系统"形态动力平衡"的唯象状态函数。
- 平衡态 /
- 沉积动力结构 /
- 信息熵 /
- 状态函数 /
- 三角洲 /
- 珠江
Abstract: From the perspective of interdisciplinary study, a brief review is conducted on the concept of "equilibrium" essential for the disciplines that the estuarine and coastal studies are closely related to. Based on output of the morphodynamic model PRD-LTMM, the water depth and corresponding area are selected as the state variables to construct the probability spaces that are used to calculate information entropy of the sub-delta systems. By comparing evolution of the depositional dynamic structures, which are briefly sketched in the context,and the geomorphic information entropy, it is found that the information entropy can be used as a phenomenological state function of the "morphodynamc equilibrium" in a given sense.
- equilibrium /
- depositional dynamic structures /
- information entropy /
- state function /
- delta /
- Zhujiang River

HTML全文

参考文献(52)

von Elverfeldt K. System Theory in Geomorphology:Challenges, Epistemological Consequences and Practical Implications[M]. New York:Springer, 2012:1-142.

Scheidegger A E. Limitations of system approach in geomorphology[J]. Geomorphology, 1992, 5(3/5):213-217.

李炎. 均衡态:动力-沉积-地貌系统的跨尺度联系[J]. 海洋学报, 2018, 40(7):38-42. Li Yan. The equilibrium status:a cross-scale linkage for hydrodynamics, sedimentology, and geomorphology[J]. Haiyang Xuebao, 2018, 40(7):38-42.

O'Brien M P. Estuary tidal prisms related to entrance areas[J]. Civil Engineering, 1931, 1(8):738-739.

O'Brien M P. Equilibrium flow areas of inlets on sandy coasts[J]. J. Waterw. Harbors Coastal Eng. Div. Am. Soc. Civ. Eng., 1969, 95:43-52.

Jarrett J T. Tidal prism-inlet area relationships[R]. GITI Report 3, U.S. Army Engineering Waterways Experiment Station, Vicksburg, Mississippi, USA.1976:33.

Davidson M A, Turner I L. A behavioral template beach profile model forpredicting seasonal to interannual shoreline evolution[J]. Journal of Geophysical Research, 2009, 114:F01020.

Davidson M A, Lewis R P, Turner I L. Forecasting seasonal to multi-year shoreline change[J]. Coastal Engineering, 2010, 57:620-629.

Davidson M A, Splinter K D, Turner I L. A simple equilibrium model forpredicting shoreline change[J]. Coastal Engineering, 2013, 73:191-202.

Frazer L N, Anderson T R, Fletcher C H. Modeling storms improves estimates of long-term shoreline change[J]. Geophysical Research Letters, 2009, 36:L20404.

Miller J K, Dean R G. A simple new shoreline change model[J]. Coastal Engineering, 2004, 51:531-556.

Yates M L, Guza R T, O'Reilly W C. Equilibrium shoreline response:observationsand modeling[J]. Journal of Geophysical Research, 2009, 114:C09014.

Splinter K D, Turner I L, Davidson M A. How much data is enough? The importance of morphological sampling interval and duration for calibration of empirical shoreline models[J]. Coastal Engineering, 2013, 77:14-27.

Dastgheib A, Roelvink J A, Wang Z B. Long-term process-based morphological modeling of the Marsdiep Tidal Basin[J]. Marine Geology, 2008, 256:90-100.

高抒. 东海沿岸潮汐汊道的P-A关系[J]. 海洋科学, 1988(1):15-19. Gao Shu. P-A relations of tidal inlets along the East China Sea Coast[J]. Marine Sciences, 1988(1):15-19.

夏小明. 三门湾潮汐汊道系统的稳定性[D]. 杭州:浙江大学, 2011. Xia Xiaoming. Stability of tidal inlet in the Sanmen Bay[D]. Hangzhou:Zhejiang University, 2011.

De Vriend H J. Mathematical modelling of meso-tidal barrier island coasts. part Ⅰ:Emperical and semi-emperical models[M]//Advances in Coastal and Ocean Engineering. World Sci.Hackensack, N.J., 1996:115-149.

钱宁, 张仁, 周志德. 河床演变学[M]. 北京:科学出版社, 1987. Qian Ning, Zhang Ren, Zhou Zhide. Riverbed Evolution[M]. Beijing:Science Press, 1987.

周筑宝. 对徐国宾、杨志达两先生某些论点的讨论[J]. 水利学报, 2014, 45(1):122-125. Zhou Zhubao. Discussion on some arguments of Xu Guobin and Yang Zhida[J]. Journal of Hydraulic Engineering, 2014, 45(1):122-125.

徐国宾, 杨志达. 对周筑宝先生讨论意见的答复[J]. 水利学报, 2014, 45(8):1004-1008. Xu Guobin, Yang Zhida. Reply to Zhou Zhubao's discussion[J]. Journal of Hydraulic Engineering, 2014, 45(8):1004-1008.

陈绪坚, 胡春宏. 河流最小可用能耗率原理和统计熵理论研究[J]. 泥沙研究, 2004(6):10-15. Chen Xujian, Hu Chunhong. Research on the theory of minimum rate of available energy dissipation and statistic entropy in rivers[J]. Journal of Sediment Research, 2004(6):10-15.

Yang C T, Song C C S. Theory of minimum rate of energy dissipation[J]. Journal of the Hydraulics Division, ASCE,1979, 105(7):769-784.

Yang C T, Song C C S. Hydraulic geometry and minimum rate of energy dissipation[J]. Water Resources Research, 1981, 17(4):1014-10181.

周筑宝. 最小耗能原理及其应用[M]. 北京:科学出版社, 2001. Zhou Zhubao. The principle of minimum energy consumption and its application[M]. Beijing:Science Press, 2001.

徐国宾, 练继建. 河流调整中的熵、熵产生和能耗率的变化[J]. 水科学进展, 2004, 14(1):1-5. Xu Guobin, Lian Jijian. Changes of the entropy, the entropy production and the rate of energy dissipation in river adjustment[J]. Advances in Water Research, 2004, 14(1):1-5.

徐国宾, 杨志达. 基于最小熵产生与耗散结构和混沌理论的河床演变分析[J]. 水利学报, 2012, 43(8):948-956. Xu Guobin, Yang Zhida. Analysis of river bed changes based on the theories of minimum entropy production dissipative structure and chaos[J]. Journal of Hydraulic Engineering, 2012, 43(8):948-956.

Chang H H. Minimum stream power and river channel patterns[J]. Journal of Hydrology, 1979, 41:303-327.

Strahler A N. Equilibrium theory of erosional slopes, approached by frequency distribution analysis[J]. American Journal of Science, 1950, 248:673-696.

Strahler A N. Dynamic basis of geomorphology[J]. Geological Society of America Bulletin, 1952, 63:923-938.

Strahler A N. Statistical analysis in geomorphic research[J]. The Journal of Geology, 1954, 62(1):1-25.

Culling W E H. Multicyclic streams and the equilibrium theory of grade[J]. The Journal of Geology, 1957, 65(3):259-274.

Chorley R. Geomorphology and general system theory[M]. Washinton:United States Government Printing Office, 1962:1-10.

Chorley R J, Kennedy B A. Physical Geography:A Systems Approach[M]. London:Prentice Hall, 1971:1-370.

Huggett R J. Fundamentals of Geomorphology[M]. New York:Taylor& Francis e-Library, 2007:1-458.

Phillips J D. Evolutionary geomorphology:thresholds and nonlinearity in landform response to environmental change[J]. Hydrology and Earth System Sciences, 2006, 3(10):365-394.

尹国康. 系统论思想在地貌学中的应用[J]. 地理学报, 1991, 46(1):26-34. Yin Guokang. Application of systems theory in geomorphology[J]. Acta geographica Sinica, 1991, 46(1):26-34.

李政道. 统计力学[M]. 上海:上海科学技术出版社, 2006:1-202. Li Zhengdao. Statistic Mechanics[M]. Shanghai:Shanghai Science and Technology Press, 2006:1-202.

林宗涵. 热力学与统计力学[M]. 北京:北京大学出版社, 2007:1-637. Lin Zonghan. Thermodynamics and Statistic Mechanics[M]. Beijing:Peking University Press, 2007:1-637.

李如生. 非平衡热力学和耗散结构[M]. 北京:清华大学出版社, 1986:1-407. Li Rusheng. Nonequilibrium thermodynamics and dissipative structure[M]. Beijing:Tsinghua University Press, 1986:1-407.

Nicolis G, Prigojine I. Self-Organization in Non-equilibrium Systems[M]. John Wiley & Sons, 1977.

冯端. 溯源探幽:熵的世界[M]. 北京:科学出版社出版, 2009:1-293. Feng Duan. Tracing the Source:the World of Entropy[M]. Beijing:Science Press, 2009:1-293.

徐俊鸣. 珠江三角洲[M]. 广州:广东人民出版社, 1973:1-88. Xu Junming. Zhujiang Delta[M]. Guangzhou:Guangdong People's Press, 1973:1-88.

吴超羽, 包芸, 任杰, 等. 珠江三角洲及河网形成演变的数值模拟和地貌动力学分析:距今6000~2500 a[J]. 海洋学报, 2006, 28(4):64-80. Wu Chaoyu, Bao Yun, Ren Jie, et al. A numerical simulation and mophodynamic analysis on the evolution of the Zhujiang River Delta:6000-2500 a BP[J]. Haiyang Xuebao, 2006, 28(4):64-80.

吴超羽, 任杰, 包芸, 等.珠江河口"门"的地貌动力学初探[J]. 地理学报. 2006, 61(5):537-548. Wu Chaoyu, Ren Jie, Bao Yun, et al. A preliminary study on the morphodynamic evolution of the ‘gate’ of the Pearl River Delta, China[J]. Acta Geographica Sinica, 2006, 61(5):537-548.

Wu Chaoyu, Wei Xing, Ren Jie, et al. Morphodynamics of the rock-bound outlets of the Pearl River estuary, South China-A preliminary study[J]. Journal of Marine Systems, 2010, 82:S17-S27.

Wu Chaoyu, Zhou Di. Long-term morpho-dynamics in a special type of estuary[J]. Science in China:Series B, 2001, 44(S):112-125.

Wei Xing, Wu Chaoyu. Long-term process-based morphodynamic modeling of the Pearl River Delta[J]. Ocean Dynamics, 2014, 64(12):1753-1765.

吴超羽,何志刚,任杰, 等. 珠江三角洲中部子平原形成演变机理研究——以大鳌平原为例[J]. 第四纪研究, 2007, 27(5):814-827. Wu Chaoyu, He Zhigang, Ren Jie, et al. Physical study on the evolution of the sub-deltaic plains in the mid Zhujiang River Delta:a case study of Da'ao Sub-delta[J]. Quaternary Sciences, 2007, 27(5):814-827.

韦惺. 全新世以来珠江三角洲的沉积演变模式研究[D]. 广州:中山大学, 2010. Wei Xing. A study of the Holocene sedimentary evolution pattern of the Pearl River Delta[D]. Guangzhou:Sun Yat-sen University, 2010.

Mann H B. Nonparametic tests against trend[J]. Econmometrica, 1945, 13:245-259.

Kendall M G. Rank Correlation Methods[M]. London:C. Groffin, 1948.

余东华. 6000-2500 a BP珠江三角洲西江主干河道发育演变及其数值模拟研究[D]. 广州:中山大学, 2010. Yu Donghua. A numerical simulation and mophodynamic analysis on the evolution of the Xijiang main channel since 6000-2500 a BP[D]. Guangzhou:Sun Yat-sen University, 2010.

施引文献

资源附件(0)

访问统计