岩溶地下水灰色系统分析软件开发

王亚捷; 郝永红; 王学萌; 李华敏; 赵娇娟

doi:10.3969/j.issn.1001-4810.2010.04.007

岩溶地下水灰色系统分析软件开发

doi: 10.3969/j.issn.1001-4810.2010.04.007

1.
天津师范大学计算机与信息工程学院
2.
天津师范大学天津市水环境与水资源重点实验室
3.
山西省农业科学院综合考察所
4.
天津师范大学城市与环境科学学院

基金项目: 国家自然科学基金(40972165,40572150)、天津市自然科学基金09JCYBJC27500、环境地球化学国家重点实验室开放基金

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出版历程
- 收稿日期: 2010-06-09
- 发布日期: 2010-12-25

Grey system analysis software development for karst ground water modeling

1.
College of Computer and Information Engineering, Tianjin Normal University
2.
Key Lab of Water Environmentand Water Resources, Tianjin Normal University
3.
Institute of Agriculture Resources Surveyof Shanxi Province
4.
College of Urbanand Environmental Sciences, Tianjin Normal University

摘要

摘要: 结合灰色系统在岩溶地下水方面的研究进展,从实际应用的角度出发,通过逐步求精的方法,使用VisualC++6.0编程,开发出一套能够满足水文地质工作者使用且操作方便的岩溶地下水灰色系统分析软件。该软件分别由灰色关联分析、数据预处理、GM(1,1)模型、等维递补预测、残差周期模型和GM(1,N)预测模型6个模块组成,具有操作简单便捷、计算结果精确、出错信息处理完善、预测结果直观、数据输入输出方式灵活、残差结果曲线输出及可推广性强等优点。利用该软件对山西柳林泉2008和2009年的泉水流量进行预测检验,GM(1,1)模型的残差周期修正预测精度明显提高,2008年的预测误差由0.32m3/s下降到0.17m3/s,2009年的预测误差由0.29m3/s下降低到0.19m3/s。
- 岩溶地下水 /
- 流量预测 /
- 灰色系统 /
- 软件工程
Abstract: After analyzed recent application of grey system theory in karst hydrology, a grey system modeling software is developed by means of step wise refinement method and VisualC++ 6.0 with the thoughts of software engineering. There are six modules in the software including grey relational analysis, data pretreatment, grey relational analysis, GM(1,1) model, dimension-fixed and recursion-compensated prediction model, GM(1,1) decomposition model, and GM(1,N) model as well. It is object-oriented and easy to operate, and able to meet the needs of hydrologists for groundwater simulation. This paper describes the software's design process, analyzes the functions and implementation of each module, presents the software examination process, and states the software's benefits on the basis of a case study in Liulin Springs, Shanxi, China. AGM(1,1) model is set up for Liulin Springs in light of the spring discharge data from 1971 to 2007, and the model is verified by spring discharge data in 2008 and 2009. The results show that the residuals errors decrease from 0.32 m3/s to 0.17m3/s in 2008 and from 0.29m3/s to 0.19m3/s in 2009 by periodic correction to the residuals.
- karst groundwater /
- discharge prediction /
- grey system /
- software engineering

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参考文献(26)

[1]	JaquetO,SiegelP,KlubertanzG,etal.Stochasticdiscretemodelofkarsticnetworks［J］.AdvanceinWaterResources,2004,27:751-760.
[2]	袁道先.中国岩溶学［M］.北京:地质出版社,1993.
[3]	韩行瑞,梁永平.北方岩溶地区水资源科学调配［J］.中国岩溶,1989,8(2):200-207.
[4]	HaoYH,YehTCJ,HuCH,etal.Karstgroundwaterman-agementbydefiningprotectionzonesbasedonregionalgeolog-icalstructuresandgroundwaterflowfields［J］.EnvironmentalGeology,2006,50(3):415-422.
[5]	QuinlanJF,DaviesGJ,JonesSW,etal.Theapplicationofnumericalmodelstoadequatelycharacterizedground-waterflowinkarsticandothertriple-porosityaquifers.［C］//RitchyJD,RumbaughJO(Eds.),SubsurfaceFluid-flow(Ground-WaterandVadoseZone)Modeling,ASTMSTP1288,AmericanSoci-etyforTestingandMaterials,1996:114-133.
[6]	LabatD,AbabouR,ManginA.Linearandnonlinearinput/out-putmodelsforkarsticspringflowandfloodpredictionatdiffer-enttimescales［J］.StochasticEnvironmentalResearchandRiskAssessment,1999,13:337-364.
[7]	HaoYH,ZhuYE,ZhaoY,etal.Theroleofclimateandhu-maninfluencesinthedry-upoftheJinciSprings,China［J］.JournaloftheAmericanWaterResourcesAssociation,2009,45(5):1228-1237.
[8]	HaoYH,SunQX,WuJ,etal.Estimatingclimateandhu-maneffectsonkarstspringsdischargeusingARIMAXmodel［J］.GroundWater(Underreview).
[9]	HaoYH,LiuGL,LiHM,etal.Investigationofkarstichydrologicalprocessesusingwaveletanalyses［J］.HydrogeologyJournal(Underreview).
[10]	郭纯青.岩溶地下水评价灰色系统理论与方法研究［M］.北京:地质出版社,1993:4-8.
[11]	HaoYH,YehTCJ,GaoZQ,etal.Agraysystemmodelforstudyingtheresponsetoclimaticchange:theLiulinkarstspring,China［J］.JournalofHydrology,2006,328(3-4):668-676.
[12]	HaoYH,YehTCJ,WangYR,etal.Analysisofkarstaq-uiferspingfolwswithagraysystemdecompositionmodel［J］.GroundWater,2007,45(1):46-52.
[13]	HaoYH,WangYJ,ZhuYE,etal.Responseofkarstspringstoclimatechangeandanthropogenicactivities:theNiangziguanSprings,China［J］.ProgressinPhysicalGeogra-phy,2009,33(5):634-649.
[14]	郝永红,王玮,王国卿,等.气候变化及人类活动对中国北方岩溶泉的影响［J］.地质学报.2009,83(1):139-144.
[15]	夏军.灰色系统水文学［M］.武汉:华中理工大学出版社,2000:24-53.
[16]	郝永红,黄登宇,张文忠,等.山西神头泉流量的灰色预测模型研究.水利学报.2004,(1):111-114.
[17]	ShapiroAM,HsiehPA.Howgoodareestimatesoftransmis-sivityfromslugtestsinfracturerock?GroundWater.1998.36(1):37-48.
[18]	刘思峰,党耀国,方志耕,等.灰色系统理论及其应用［M］.北京:科学出版社,2004:5-8.
[19]	肖新平,宋中民,李峰.灰技术基础及其应用［M］.北京:科学出版社,2005.
[20]	王学萌,聂宏声.灰色系统模型在农村经济中的应用［M］.武汉:华中理工大学出版社,1989.
[21]	王学萌.等维灰数递补动态预测［J］.华中工学院学报,1989,4:9-16.
[22]	WangYJ,HaoYH,WangXM.Simulationofkarsthydro-logicalprocessesusingGM(1,1)metabolicmodel［C］.Pro-ceedingsof2009IEEEInternationalConferenceGreySystemsandIntelligentServices,Nanjing,China,2009:598-603.
[23]	张海藩.软件工程导论［M］.北京:清华大学出版社,2003:45-173.
[24]	GB/T9385-2008计算机软件需求规格说明规范［S］.北京:中国标准出版社,2008.
[25]	钱能.C++程序设计教程［M］.北京:清华大学出版社,2005.
[26]	GB/T15532-2008计算机软件测试规范［S］.北京:中国标准出版社,2008.