黄河断流成因与对策研究
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摘要
从地球科学“人为地质作用理论”出发 ,分析了黄河下游断流的严重性与危害性后认为 ,黄河下游断流不仅对黄河流域及整个中国生态环境产生重大影响 ,而且对社会经济发展以及可持续发展产生严重后果。在探讨了黄河下游断流的成因后认为 ,黄河下游断流有自然的原因和人为的原因 ,其中人类活动、人类工程活动及其人为地质作用的负面影响是黄河断流最主要的原因之一 ,从而提出解决黄河下游断流的科学对策 ,包括科学保护、科学开发、科学利用水资源以及暂缓实施南水北调中、西线工程等的若干建议
Based on the man made geological process of geosciences, this paper discusses the serious consequences and perniciousness of the cutoff in the lower reaches of the Yellow River. It suggests that the cutoff would have a great effect on both the ecological environment of the whole country as well as the Yellow River Basin and the development as well as the sustainable development in socioeconomics. On the basis of the analysis of the genesis, it shows that the cutoff results from both natural and man made processes , in which the negative effects caused by man activities, man engineering activities, and man made geological processes play the most important part. The paper also gives the scientific countermeasures on the cutoff, which include the suggestions of protecting, developing, and utilizing the water resources in China scientifically.
Based on the man made geological process of geosciences, this paper discusses the serious consequences and perniciousness of the cutoff in the lower reaches of the Yellow River. It suggests that the cutoff would have a great effect on both the ecological environment of the whole country as well as the Yellow River Basin and the development as well as the sustainable development in socioeconomics. On the basis of the analysis of the genesis, it shows that the cutoff results from both natural and man made processes , in which the negative effects caused by man activities, man engineering activities, and man made geological processes play the most important part. The paper also gives the scientific countermeasures on the cutoff, which include the suggestions of protecting, developing, and utilizing the water resources in China scientifically.
引文
[1]蔡学林.加强人为地质作用研究与教学[J].成都:成都理工学院档案馆,1994.
[2]蔡学林.环境与人类[A].中国环境保护全书[C].北京:中国人事出版社,1998.507-523.
[3]蔡学林,朱介寿,阳正熙,等.资源环境与21世纪地球科学发展趋势[J].成都理工学院学报,2000,27(3):221-235.
[4]王建中,王玲,石国安.黄河断流情况及对策[J].中国水利,1999,(4):10-13.
[5]任美锷.黄河下游断流引起的环境问题及其防治措施[J].科技导报,1999,(2):3-6.
[6]郝明德.黄河断流与黄河流域综合治理[J].人民黄河,2000,22(5):4-8.
[7]张新三.黄河下游断流与调水问题的阅读与思考[J].科技导报,2000,(2):28-31.
[8]刘传正.论黄河下游断流问题[J].中国区域地质,1999,18(4):418-424.
[9]新华社.黄河源头出现断流,生态环境严重恶化[N].西安晚报,1998-10-29.
[10]崔树彬.渠化黄河河道与黄淮海平面可持续发展探讨[J].科技导报,2000,(2):22-26.
[11]张启舜.黄河断流的现象和实质[J].科技导报,1999,(2):12-14.
[12]洪文之,王健.“引大”工程与大通河谷沦为荒漠的危险性浅析[J].水文地质工程地质,1996,(4):44.
[13]王思敬.论人类工程活动与地质环境的相互作用及其环境效应[J].地质灾害与环境保护,1997,8(1):19-26.
[14]蔡学林,方向池.公路水毁地质灾害及其防治战略研究[J].自然灾害学报,1999,8(2):181-187.
[15]中国科学院,中国工程院.加快西北地区发展的几个关键问题[J].地球科学进展,2000,15(5):489-498.
[16]张岳.21世纪我国水利面临的十大挑战[J].中国水利,2000,(1):13-15.
[17]彭泽云,阎勇军,张明政.我国南水北调应以系统工程的观点重新规划[J].科技导报,2000,(5):51-54.
[18]高季章,甘泓,沈大军.黄河断流与西部调水[J].科技导报,1999,(2):15-18.
[19]赵衍庚.南水北调新东线立足于长江丰水汛期[J].科技导报,1999,(2):19-22.
[20]章淹,谯秀蓉,林锦瑞.南水北调中线重大水旱变化及其影响[J].科技导报,2000,(2):16-20.
[21]贾绍风.必须深入进行南水北调工程的经济可行性论证[J].科技导报,2001,(7):17-20.
[22]张新海,张玫,韩侠,等.南水北调西线工程对长江的影响初步分析[J].人民黄河,2000,22(2):20-22.
[23]李林,张国胜,汪青,等.黄河上游流域蒸散量及其影响因子分析[J].地球科学进展,2000,15(3):256-259.
[24]陈梦熊.中国水文地质环境地质问题研究[M].北京:地震出版社,1998.30-37.
[25]陈西庆,陈吉余.关于研究与控制长江枯季入海流量下降趋势的建议[J].科技导报,2000,(2):39-40.
[26]袁志梅,吴霞芬.中国21世纪水资源的前景及对策[J].地质论评,2000,46(4):422.
[2]蔡学林.环境与人类[A].中国环境保护全书[C].北京:中国人事出版社,1998.507-523.
[3]蔡学林,朱介寿,阳正熙,等.资源环境与21世纪地球科学发展趋势[J].成都理工学院学报,2000,27(3):221-235.
[4]王建中,王玲,石国安.黄河断流情况及对策[J].中国水利,1999,(4):10-13.
[5]任美锷.黄河下游断流引起的环境问题及其防治措施[J].科技导报,1999,(2):3-6.
[6]郝明德.黄河断流与黄河流域综合治理[J].人民黄河,2000,22(5):4-8.
[7]张新三.黄河下游断流与调水问题的阅读与思考[J].科技导报,2000,(2):28-31.
[8]刘传正.论黄河下游断流问题[J].中国区域地质,1999,18(4):418-424.
[9]新华社.黄河源头出现断流,生态环境严重恶化[N].西安晚报,1998-10-29.
[10]崔树彬.渠化黄河河道与黄淮海平面可持续发展探讨[J].科技导报,2000,(2):22-26.
[11]张启舜.黄河断流的现象和实质[J].科技导报,1999,(2):12-14.
[12]洪文之,王健.“引大”工程与大通河谷沦为荒漠的危险性浅析[J].水文地质工程地质,1996,(4):44.
[13]王思敬.论人类工程活动与地质环境的相互作用及其环境效应[J].地质灾害与环境保护,1997,8(1):19-26.
[14]蔡学林,方向池.公路水毁地质灾害及其防治战略研究[J].自然灾害学报,1999,8(2):181-187.
[15]中国科学院,中国工程院.加快西北地区发展的几个关键问题[J].地球科学进展,2000,15(5):489-498.
[16]张岳.21世纪我国水利面临的十大挑战[J].中国水利,2000,(1):13-15.
[17]彭泽云,阎勇军,张明政.我国南水北调应以系统工程的观点重新规划[J].科技导报,2000,(5):51-54.
[18]高季章,甘泓,沈大军.黄河断流与西部调水[J].科技导报,1999,(2):15-18.
[19]赵衍庚.南水北调新东线立足于长江丰水汛期[J].科技导报,1999,(2):19-22.
[20]章淹,谯秀蓉,林锦瑞.南水北调中线重大水旱变化及其影响[J].科技导报,2000,(2):16-20.
[21]贾绍风.必须深入进行南水北调工程的经济可行性论证[J].科技导报,2001,(7):17-20.
[22]张新海,张玫,韩侠,等.南水北调西线工程对长江的影响初步分析[J].人民黄河,2000,22(2):20-22.
[23]李林,张国胜,汪青,等.黄河上游流域蒸散量及其影响因子分析[J].地球科学进展,2000,15(3):256-259.
[24]陈梦熊.中国水文地质环境地质问题研究[M].北京:地震出版社,1998.30-37.
[25]陈西庆,陈吉余.关于研究与控制长江枯季入海流量下降趋势的建议[J].科技导报,2000,(2):39-40.
[26]袁志梅,吴霞芬.中国21世纪水资源的前景及对策[J].地质论评,2000,46(4):422.
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