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Possibilities and limits in the management of mountain watersheds: Lessons from the Maya civilization

机译:山地流域管理中的可能性和限制:玛雅文明的课程

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This study focused on three pre-Columbian centres of the Maya society: Kaminaljuyu, Copan and Tikal. Historical method was used to compare their development in relation to the hydrological regime. Kaminaljuyu is based on a catchment-lake relationship, Copan on a downstream impact of a large mountain watershed, and Tikal represents an upland settlement based on a headwater spot. The main aim is to analyse water management of these centres, particularly, in view of their rise and collapse. Selected ancient Maya centres used very sophisticated water management systems with several signs of environmental and social implications. That water technology ensured their economic prosperity and consolidation of the administrative and political power for a long time. The water supply of the Maya settlement faced a serious impact of seasonal rainfall with relatively long dry periods (4-5 months) as well as fast runoff formation in the karstified bedrock. While in the Copan centre, surrounded by a large mountain watershed, the flood control was the highest priority, headwater located Kaminaljuyu and Tikal concentrated mainly on the harvest and storage of rain water. Later, these centres had to adapt to the increasing population, changing society, environment and landuse. For a long time their water management was able to adapt to the increasing demand of water and decreasing recharge of water resources. The exact reason of the collapse of these Maya centres was probably a superposition of the climate change, overexploitation of natural resources, and exceeding the carrying capacity of their environment. All those societies reached an extremely high level of hydraulic engineering, but, they were still limited in knowledge of hydrology and watershed management. Finally, it was probably a series of extreme droughts leaded to their final collapse.
机译:本研究专注于玛雅社会的三个哥伦比亚中心:Kaminaljuyu,Copan和Tikal。历史方法用于比较其与水文制度相关的发展。 Kaminaljuyu基于一个集水湖关系,Copan对大型山地流域的下游影响,而蒂克尔代表了基于地图的高地沉降。主要目的是分析这些中心的水资源,特别是考虑到他们的崛起和崩溃。选定的古代玛雅中心使用了非常复杂的水管理系统,具有几个环境和社会影响的迹象。水技术确保了他们经济繁荣和长期巩固行政和政治权力。玛雅沉降的供水面临着季节性降雨的严重影响,干燥时期(4-5个月)以及喀证精确的基岩中的快速径流形成。虽然在科潘中心环绕着大型山地流域,但洪水控制是最优先的优先级,位于Kaminaljuyu和Tikal主要集中在雨水中的收获和储存。后来,这些中心必须适应增加人口,改变社会,环境和土地利用。长期以来,他们的水管理能够适应日益增长的水需求和降低水资源充电。这些玛雅中心崩溃的确切原因可能是气候变化的叠加,对自然资源的过度开采,并超出了其环境的承载能力。所有这些社会都达到了极高的水力工程水平,但是,他们仍然有限于水文和流域管理。最后,这可能是一系列极端干旱引领他们的最终崩溃。

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