Chaotic characters of dynamic system of the Yellow River basin from sandiness time series:an integrative research attempt to geographic system
Received date: 2006-05-08
Revised date: 2006-09-20
Online published: 2006-12-15
The sandiness content on every section of the Yellow River relates all the factors that are interactive in many ways,so it includes some evolution information of the system controlled by monitoring section.We can infer the dynamic characters of the system from the sandiness time series based on the techniques of phase space reconstruction and the picking-up methods for chaos indexes.Sandiness contents from 1952 to 2000 were chosen as the time series on Toudaoguai section,Tongguan section,Huayuankou section and Lijin section along the Yellow River.Correlation dimension(D2) was calculated according to Grassberger-Procaccia arithmetic,Kolmogorov entropy(K2) according to Zhao Gui-bing arithmetic,and Hurst index(H) according to Rescaled Range Analysis(R/S).The results are shown as follows:(1) The correlation dimension on Toudaoguai section is 3.24,Tongguan section is 5.69,Huayuankou section is 6.57 and Lijin section is 7.34.We can see that all the dimensions are fractal dimensions,so the dynamic systems controlled by different sections of the Yellow River basin are chaotic systems and the chaotic degrees heighten gradually from upper section to lower section.(2) Forecast time of the time series was calculated by 1/K2.On Toudaoguai section,the forecast time of the sandiness time series is about 8 years,and the other sections are 3 years.The more obvious the chaos is,the shorter the forecast time is.(3) Hurst indexes on all the study sections are more than 0.5, the maximum is 0.86 on Tongguan section and the minimum is 0.68 on Toudaoguai section,which indicates that the changes of the time series have persistence trends in the average forecasting time.The past trends of the time series from 1952 to 2000 on all the sections were wavelike descending,so that the future trends of the time series will go on wavelike descending too.Compared with the time series from 1999 to 2000,the future trends was validated with the time series from 2001 to 2004 on Tongguan section,Huayuankou section and Lijin section.(4) We can get some information from correlation dimensions and saturated inlay dimensions to construct useful dynamic system model.The sandiness time series on Lijin section infers the dynamic characters of the whole Yellow River basin,its correlation dimension is 7.34 and the saturated inlay dimension is 10.Therefore,the dynamic model of the whole Yellow River basin needs eight state variables and two control variables at least.A general form of the dynamic model of the whole Yellow River basin was given in this paper.
MA Jian-hua,CHU Chun-jie . Chaotic characters of dynamic system of the Yellow River basin from sandiness time series:an integrative research attempt to geographic system[J]. GEOGRAPHICAL RESEARCH, 2006 , 25(6) : 949 -958 . DOI: 10.11821/yj2006060001
[1] B索恰瓦地理系统学说导论李世玢译北京:商务印书馆,199.
[2] 吴传钧,张家桢我国20世纪地理科学发展回顾及新世纪前景展望地理学报,1999,54(5):385~390
[3] 陆大道关于地理学人地系统!理论研究地理研究,2002,21(2):135~145
[4] 陆大道中国地理学发展若干值得思考的问题地理学报,2003,58(1):2~8
[5] 葛全胜,吴绍洪,朱立平,等.世纪中国地理学发展的若干思考地理研究,2003,22(4):406~415
[6] 倪绍祥地理学综合研究的新进展地理科学进展,2003,22(4):335~34.
[7] 杨勤业,郑度,吴绍洪,等20世纪50年代以来中国综合自然地理学研究进展地理研究,2005,24(6):899~910
[8] 蔡运龙,陆大道,周一星,等地理科学的中国进展与国际趋势地理学报,2004,59(6):803~810
[9] 宋长青,冷疏影21世纪中国地理学综合研究的主要领域地理学报,2005,60(4):546~552
[10] 黄秉维自然地理学一些主要的趋势地理学报,1960,26(3):149~154
[11] ,黄秉维文集?编辑组自然地理工作六十年黄秉维文集北京:科学出版社,1993
[12] 黄秉维,郑度,赵名茶现代自然地理北京:科学出版社,1999
[13] 美国国家航空和宇航管理局地球系统科学委员会地球系统科学陈泮勤等译北京:地震出版社,1992
[14] 黄秉维可持续发展战略的理论基础建立地球系统科学的基本设想中国环境报,1996 04 13
[15] 黄秉维论地球系统科学与可持续发展战略科学基础地理学报,1996,51(4):350~356
[16] 黄秉维区域可持续发展的理论基础陆地系统科学地理学报,1996,51(5):445~453
[17] 杨勤业地理综合研究与陆地系统科学祝黄秉维院士八十五寿辰地理研究,1997,16(4):1~6
[18] ,地理学报?编辑部地球系统科学庆贺黄秉维院士八十五华诞地理学报,1998,53(1):1~12
[19] 吕金虎,陆君安,陈士华混沌时间序列分析及其应用武汉:武汉大学出版社,2002
[20] 赵贵兵,石炎福,等从混沌时间序列同时计算关联维和K olm ogorov熵计算物理,1999,16(3):309~315
[21] 马建华,管华系统科学及其在地理学中的应用北京:科学出版社,2002
[22] 许炯心黄河下游历史泥沙灾害的宏观特征及其与流域因素和人类活动的关系历史气候及植被因素的影响.自然灾害学报,2001,10(2):7~1.
[23] 许炯心黄河下游历史泥沙灾害的宏观特征及其与流域因素和人类活动的关系人类活动、历史地震及地形因子的影响自然灾害学报,2001,10(3):7~12
[24] 许炯心流域因素与人类活动对黄河下游河道输沙功能的影响中国科学(D辑),2004,38(8):775~78.
[25] 许炯心无定河流域侵蚀产沙过程对水土保持措施的响应地理学报,2004,59(6):972~98.
[26] 金德龙,师长兴,陈浩,等人为动力泥沙灾害类型及其特征研究地理科学进展,2000,19(4):317~326
[27] 景可,等我国土壤侵蚀与地理环境的关系地理研究,1999,9(2):29~38
[28] 卢金发黄河中游流域地貌形态对流域产沙的影响地理研究,2002,21(2):171~178
[29] 陈浩,等黄河中游流域环境要素对水沙变异的影响地理研究,2002,21(2):179~187
[30] 卢金发土地覆被对黄河中游流域泥沙产生的影响地理研究,2003,22(5):571~578
[31] 王文均,叶敏,陈显维长江径流时间序列混沌特性的定量分析水科学进展,1994,5(2):87~94
[32] 王良健,彭补拙分形方法在洪涝灾害预测中的应用以广西梧州为例地理科学,1998,18(3):242~248
[33] 周寅康,包浩生,张捷淮河流域洪涝变化混沌演化特征研究地球信息科学,1999,1(2):8~1.
[34] 周寅康,王腊春,许有鹏,等淮河流域洪涝变化动力系统研究地理科学,2001,21(1):41~45
[35] 魏一鸣,等1949~1994年中国洪水灾害成灾面积的时序分形特征自然灾害学报,1998,7(1):83~86,93
[36] 马建华,楚纯洁花园口断面年径流量时间序列混沌特性分析人民黄河,2006,28(1):18~20
[37] Packard N H,Crut ch field J R,Farmer J D,e t al G eomet ry fr om a t im e seri es Phys R ew Let t,1980,45(9):712~716
[38] G rassb erger P,Procaccia I Ch aract erizat ion of st range at t ract ors Phys R ew Let t,1983,50(5):346~349
[39] Grass berg er P,Procaccia I Est imat ion of t he K olm ogorov ent ropy f rom a chaot ic signal Phys R ew A,1983,28(4):2591~2593
[40] Feder J Fractals N ew Y ork:Plenum Pres s,1988
[41] 黄登仕,李自强分形几何学、R/S分析与分式布朗运动自然杂志,1990,13(8):477~482
[42] C oh en A,Procaccia I Com put ing t h e K olm og or ov ent ropy from t ime signals of dissi pat ive conservat ive dynamicals yst em Phy s Rev A,1985,31(3):1872~1882
[43] 周寅康,张捷,王腊春,等长江下游地区近五百年洪涝序列的R/S分析自然资源学报,1997,6(2):78~84
[44] 郝柏林分形和分维科学杂志,1986,38(1):9~17
[45] H urs t H E Long T erm St orage:A n Experiment al St udy London:Const able,1965
[46] M andelbrot B B,Van N ess J W Fract ional br ow nian m ot ion,f racti on al noise and applicat ion S IA M R eview,1968,10:422~437
[47] M andelbrot B B,Wall is J R Some long run properti es of geographysi cal records Wat er R esour ces R es earch,1969a,5(2):321~340
[48] M andelbrot B B,Wallis J R R ob ust ness of t he rescaled range R/S in t he meas urem ent of noncycl ic long run s t at ist ical dep endence Wat er Resources Research,1969b,5(4):967~988
[49] M cheod A I,H ipel K W Pres ervati on of rescaled adju st ed range Wat er R es ou rces R esear ch,1978,14(3):491~518
[50] L orenz E N D et erminist ic nonp eriodic f low J A t mos Sci,1963,20:130~14.
[51] E N洛伦兹混沌的本质刘式达,刘式适,严中伟译北京:气象出版社,1997
[52] R ckm anm J P Ergodc th eory of chaos an d st range at t ract ors R eview M odern Phy sics,1985,57:617~655
[53] 周寅康,付重林,王腊春,等淮河流域洪涝变化可预报时间研究自然灾害学报,1999,8(4):118~122
[54] 谢正栋,等淮河流域洪水的分形特征及可预报时间研究南京大学学报(自然科学版),2003,39(1):113~119
[55] 赵晶,徐建华1950~1997年我国洪涝灾害成灾面积的分形特征研究自然灾害学报,2003,12(2):31~35
[56] h tt p//w w w yell owri ver gov cn/lib/ggl/2005 08 24/jj_160400.19297 ht ml
[57] 黄建平,衣育红利用观测资料反演非线性动力模型中国科学(B),1991,(3):331~336
[58] 彭永青,育峰,严绍瑾利用一维时间序列重建动力系统的初步研究应用气象学报,.993,4(增刊):3.~38
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