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首页> 外文期刊>Hydrogeology journal >A method for the stochastic modeling of karstic systems accounting for geophysical data: An example of application in the region of Tulum, Yucatan Peninsula (Mexico)
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A method for the stochastic modeling of karstic systems accounting for geophysical data: An example of application in the region of Tulum, Yucatan Peninsula (Mexico)

机译:解释地球物理数据的岩溶系统的随机建模方法:在尤卡坦半岛(墨西哥)图卢姆地区的应用示例

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摘要

The eastern coast of the Yucatan Peninsula, Mexico, contains one of the most developed karst systems in the world. This natural wonder is undergoing increasing pollution threat due to rapid economic development in the region of Tulum, together with a lack of wastewater treatment facilities. A preliminary numerical model has been developed to assess the vulnerability of the resource. Maps of explored caves have been completed using data from two airborne geophysical campaigns. These electromagnetic measurements allow for the mapping of unexplored karstic conduits. The completion of the network map is achieved through a stochastic pseudo-genetic karst simulator, previously developed but adapted as part of this study to account for the geophysical data. Together with the cave mapping by speleologists, the simulated networks are integrated into the finite-element flow-model mesh as pipe networks where turbulent flow is modeled. The calibration of the karstic network parameters (density, radius of the conduits) is conducted through a comparison with measured piezometric levels. Although the proposed model shows great uncertainty, it reproduces realistically the heterogeneous flow of the aquifer. Simulated velocities in conduits are greater than 1 cm s~(-1), suggesting that the reinjection of Tulum wastewater constitutes a pollution risk for the nearby ecosystems.
机译:墨西哥尤卡坦半岛的东海岸拥有世界上最发达的岩溶系统之一。由于图卢姆地区的快速经济发展以及缺乏废水处理设施,这一自然奇观正受到越来越多的污染威胁。已经开发了初步的数值模型来评估资源的脆弱性。已使用两次航空地球物理活动的数据完成了已探明洞穴的地图。这些电磁测量可以绘制未勘探的岩溶导管。网络地图的完成是通过一个随机的伪自然岩溶岩溶模拟器实现的,该模拟器先前已经开发过,但是作为本研究的一部分而进行了调整,以说明地球物理数据。连同洞穴学家的洞穴制图,将模拟网络集成到有限元流模型网格中,成为模拟湍流的管网。岩溶网络参数(密度,导管半径)的校准是通过与测得的测压水平进行比较来进行的。尽管所提出的模型显示出很大的不确定性,但它实际上再现了含水层的非均质流动。导管中的模拟速度大于1 cm s〜(-1),这表明图卢姆废水的回注对附近的生态系统构成了污染风险。

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