In this paper, the new systematical theory and methodology have been applied to the research on the structure, development and coordination of man-environment system in Jiaozuo City. It has been proved that the applic...In this paper, the new systematical theory and methodology have been applied to the research on the structure, development and coordination of man-environment system in Jiaozuo City. It has been proved that the application of self-organization theory of synergism is successful. Furthermore, on the basis of self-organization theory, a series of mathematical models have been established. The prediction of the status of man-environment system in Jiaozuo City by the year 2010, was made, and the trend of population growth, industrial development, environmental pollution were given. Finally, suggestions for the future development of Jiaozuo City were mentioned.展开更多
本文基于固城湖湖相沉积物中的元素地球化学、磁化率和粒度指标,高分辨率重建苏皖沿江平原全新世以来的水文气候变化;进而结合先秦时期考古遗址的时空分布特征,探讨研究区人地关系的演变历程。结果表明,11.5—7.0 cal ka BP期间,经历新...本文基于固城湖湖相沉积物中的元素地球化学、磁化率和粒度指标,高分辨率重建苏皖沿江平原全新世以来的水文气候变化;进而结合先秦时期考古遗址的时空分布特征,探讨研究区人地关系的演变历程。结果表明,11.5—7.0 cal ka BP期间,经历新仙女木(YD)冷干事件后,气候迅速转为最温暖湿润期,但波动频繁;7.0—5.0 cal ka BP前期气候有向冷干转变的趋势,后期气候暖湿,湖泊水位稳定;5.0—4.0 cal ka BP气候逐渐变干;4.0—1.5 cal ka BP气候波动频繁,经历“湿润—干旱—湿润”的转变过程。1.5 cal ka BP以来人类对环境的影响显著加强。上述水文气候演变过程影响了遗址的空间分布、农业发展和文化兴衰。新石器早期气候波动频繁,人类过于依赖环境,文明发展缓慢;新石器中晚期稳定的水文气候条件为农业发展奠定了生境基础,促进人口扩张;夏时期气候急剧恶化失衡,遗址数量骤减、文化衰退;商周时期水文气候恶劣,人类通过改变生产战略和技术革新以谋求自身生存和发展。随着生产力水平的提高,人地关系演变的主导因子由自然因素逐渐向人为因素倾斜,在一定限度内冷干或暖湿的气候都能推动人类文明的发展。人类从被动顺应到主动适应自然环境,体现了人类与自然环境之间的博弈过程。展开更多
文摘In this paper, the new systematical theory and methodology have been applied to the research on the structure, development and coordination of man-environment system in Jiaozuo City. It has been proved that the application of self-organization theory of synergism is successful. Furthermore, on the basis of self-organization theory, a series of mathematical models have been established. The prediction of the status of man-environment system in Jiaozuo City by the year 2010, was made, and the trend of population growth, industrial development, environmental pollution were given. Finally, suggestions for the future development of Jiaozuo City were mentioned.
文摘本文基于固城湖湖相沉积物中的元素地球化学、磁化率和粒度指标,高分辨率重建苏皖沿江平原全新世以来的水文气候变化;进而结合先秦时期考古遗址的时空分布特征,探讨研究区人地关系的演变历程。结果表明,11.5—7.0 cal ka BP期间,经历新仙女木(YD)冷干事件后,气候迅速转为最温暖湿润期,但波动频繁;7.0—5.0 cal ka BP前期气候有向冷干转变的趋势,后期气候暖湿,湖泊水位稳定;5.0—4.0 cal ka BP气候逐渐变干;4.0—1.5 cal ka BP气候波动频繁,经历“湿润—干旱—湿润”的转变过程。1.5 cal ka BP以来人类对环境的影响显著加强。上述水文气候演变过程影响了遗址的空间分布、农业发展和文化兴衰。新石器早期气候波动频繁,人类过于依赖环境,文明发展缓慢;新石器中晚期稳定的水文气候条件为农业发展奠定了生境基础,促进人口扩张;夏时期气候急剧恶化失衡,遗址数量骤减、文化衰退;商周时期水文气候恶劣,人类通过改变生产战略和技术革新以谋求自身生存和发展。随着生产力水平的提高,人地关系演变的主导因子由自然因素逐渐向人为因素倾斜,在一定限度内冷干或暖湿的气候都能推动人类文明的发展。人类从被动顺应到主动适应自然环境,体现了人类与自然环境之间的博弈过程。
