Page 48 - 2024年第55卷第6期
P. 48
1 - 10.
[29] 赵伟,王平,金菊良,等.水资源承载力评价的三元减法集对势模糊数随机模拟方法[J].华北水利水电
大学学报(自然科学版),2022,43(1):26 - 33.
[30] 金菊良,李蔓,崔毅,等.基于五元半偏减法集对势模糊数随机模拟方法的旱灾风险评估[J].华北水利
水电大学学报(自然科学版),2023,44(3):1 - 13,34.
[31] 金菊良,赵行癑,崔毅,等.半偏减法 集 对 势 在 区 域 旱 灾 风 险 评 估 中 的 应 用 [J].水 利 水 运 工 程 学 报,
2021(1):36 - 44.
[32] 金菊良,周亮广,王平,等.基于相对联系数的区域水利高质量发展评价指标体系筛选方法[J].华北水
利水电大学学报(自然科学版),2024,45(1):43 - 51.
[33] 汪哲荪,金菊良,魏一鸣,等.三角模 糊 数 随 机 模 拟 的 防 洪 工 程 联 系 数 风 险 评 价 模 型 [J].水 利 学 报,
2010,41(10):1173 - 1178.
[34] 武天欣.企业科研模式研究—从 “爱迪生象限” 到 “巴斯德象限” [D].南京:南京大学,2020.
[35] 钱学森.论技术科学[J].上海理工大学学报,2011,33(6):511 - 519.
[36] 李征,金菊良,崔毅,等.基于半偏联系数和动态减法集对势的区域水资源承载力评价方法[J].湖泊科
学,2022,34(5):1656 - 1669.
Analysisoftheoppositionrelationshipinwaterresourcesetpairsystem
1,2
3
1,2
1,2
1,2
1,2
JINJuliang ,ZHOULiangguang ,CUIYi ,WANGMingwu ,ZHOURongxing ,PANZhengwei
(1.SchoolofCivilEngineering,HefeiUniversityofTechnology,Hefei 230009,China;
2.InstituteofWaterResourcesandEnvironmentalSystemsEngineering,HefeiUniversityofTechnology,Hefei 230009,China;
3.SchoolofCivilandHydraulicEngineering,BengbuUniversity,Bengbu 233030,China)
Abstract:Theoppositionrelationshipbetweentheidentityandoppositionitemsinwaterresourcesetpairsystemis
theconcentratedreflectionofthedialecticalthinkingofwaterresourcesetpairanalysis.Itisalsothecornerstoneof
buildingconnectionnumberofsetpairsystem.Throughtheanalysisofthecorrespondingrelationshipbetweenthe
commonfivetypesofoppositionrelationshipconceptanalysisandtheirapplications ,andtheuncertaintyanalysisof
waterresourcessetpairforthefivetypesofoppositerelationshiptothesystem differenceitems ,wehavegained
someunderstandingofthecomplexandprofoundmeaningoftheoppositerelationshipasfollows.Thecommonoppo
sitesofinverseratio ,mutualexclusion,positiveandnegativetype,complementarytypeandvirtualandrealtype
inthewaterresourcessetpairsystemcanbegenerated,analyzedandcalculatedbyfuzzy,random,fluctuation,
distributionandexistenceuncertaintyvariablesrespectively.Inthesetpairsystem,themostbasicoppositionrela
tionshipsaretheinverseandmutuallyexclusiveopposition ,andthecorrespondingfuzzinessandrandomnessrefer
totheuncertaintyintermsofthecontent,nature,andnumberofresultsoftheeventoccurrence.Thechangeof
theuncertaintyofthedifferenceitemisthecauseofthechangeforthethreekindsofrelationsbetweenthesame ,
differentandoppositeintheconnectionnumber,andalsoisatypicalexpansionofthedialecticalthinkingof“one
dividedintothree”,reflectingthetransformationlawfromquantitativechangetoqualitativechange.Fuzzyuncer
taintyisthemostcommonofthefivetypesofuncertaintycharacterizedbydifferenceterms ,andtheoperationof
fuzzyuncertaintyvariablecanbeconvertedintotheoperationofrandomuncertaintyvariablethroughrandomsimula
tiontechnology.Theanalysisoffuzzyandrandom uncertaintyfocusesontheanalysisofphysicalconnotationand
mathematicalquantitativecalculationrespectively ,whichreflectsthatthedisciplineofwaterresourcesetpairanal
ysisbelongstothefieldofcomputationalthinking,andithasobviousenlighteningandguidingsignificanceforfur
therpromotingthedevelopmentoffuzzyhydrology ,stochastichydrology,waterresourcessetpairanalysis,and
structuralwaterresourcesscience.
Keywords:setpairanalysisofwaterresources;oppositionrelationship;setpairsystem;connectionnumber;
uncertaintyanalysis;dialecticalthinking;computationalthinking
(责任编辑:耿庆斋)
— 6 7 —
4