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The hydroarchaeological approach: Understanding the ancient Maya impact on the Palenque watershed.

机译:水文考古学方法:了解古代玛雅人对帕伦克流域的影响。

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摘要

Palenque, one of the best known Classic Maya centers, has what is arguably the most unique and intricate system of water management known anywhere in the Maya Lowlands. Years of archaeological research, including intensive mapping between 1997 and 2000, reveal that this major center, situated on a narrow escarpment at the base of a high mountain range in northern Chiapas, Mexico, began as a modest settlement about AD 100. Then, during the seventh and eighth centuries, Palenque experienced explosive growth, mushrooming into the second most densely populated Classic Maya center. This process of "urban" growth led to obvious changes in landcover.;In order to better understand the effects that landcover and climate change have on the availability of water for an ancient city a new approach is required. In this dissertation I introduce the hydroarchaeological approach, a new cross-disciplinary method that utilizes simulated daily paleoclimate data, watershed modeling, and traditional archaeology to view the response of the Palenque watershed to varying degrees of ancient human impact. There is great potential for watershed-climate modeling in developing plausible scenarios of water use and supply, and the effect of extreme conditions (flood and drought), all of which cannot be fully represented by atmosphere-based climate and weather projections.;One objective of this dissertation is to test the hypothesis that drought was a major cause for Palenque's collapse. Did the Maya abandon Palenque in search of water? Secondly, evaluate the hydraulic design of the water management features at Palenque against extreme meteorological events. How successful was the hydraulic engineering of the Maya in coping with droughts and floods?;The archaeological implications for this non-invasive "virtual" method are many, including detecting periods of stress within a community, estimating population limits based on the availability of water, understanding settlement patterns, as well as assisting present local populations in understanding the water cycle of Palenque.
机译:帕伦克(Palenque)是最著名的经典玛雅中心之一,拥有玛雅低地任何地方都可以称为的最独特,最复杂的水管理系统。多年的考古研究,包括1997年至2000年间的密集制图,揭示了这个主要的中心位于墨西哥北部恰帕斯州高山山脉底部狭窄的悬崖上,开始于公元100年左右。在第七和第八个世纪,帕伦克(Palenque)经历了爆炸性的增长,迅速发展成为第二大人口稠密的经典玛雅人中心。这种“城市”增长过程导致了土地覆被的明显变化。为了更好地理解土地覆被和气候变化对古代城市的水供应的影响,需要一种新的方法。在本文中,我介绍了水文考古学方法,这是一种新的跨学科方法,该方法利用模拟的每日古气候数据,分水岭建模和传统考古学来观察帕伦克分水岭对古代人类影响的不同程度的响应。在开发合理的用水和供水情景以及极端条件(洪水和干旱)的影响方面,分水岭-气候模型具有巨大潜力,而所有这些都不能完全通过基于大气的气候和天气预测来体现。本论文的目的是检验以下假设:干旱是帕伦克(Palenque)倒塌的主要原因。玛雅人放弃了帕伦克(Palenque)寻找水吗?其次,针对极端气象事件评估帕伦克水管理设施的水力设计。玛雅人的水利工程技术在应对干旱和洪水方面取得了多大的成功?;这种非侵入式“虚拟”方法的考古学意义是很多的,包括检测社区内的压力时期,根据水的可利用性估算人口极限,了解定居方式,并帮助当前的当地居民了解帕伦克的水循环。

著录项

  • 作者

    French, Kirk Dow.;

  • 作者单位

    The Pennsylvania State University.;

  • 授予单位 The Pennsylvania State University.;
  • 学科 Anthropology Archaeology.;Hydrology.;Engineering Environmental.
  • 学位 Ph.D.
  • 年度 2009
  • 页码 220 p.
  • 总页数 220
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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