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Assessment of travertine evolution in Jiuzhaigou-Huanglong areausing grey system model

机译:九寨沟 - 黄龙近灰色系统模型评估曲曲线演变

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The travertine in Huanglong has lasted for thousands of decades on account of the karst geologic effect. In recent years, the travertine came to be dried up, blacken, sanded, which seriously affected the aesthetic characteristic. We find that there are no perfecting monitoring systems and timing data by collecting and anglicizing Monitoring data. We choose grey model which requires less timing data and higher predictive results. The travertine development is predicted using the Ph factor. The whole Huanglong predictive result is based on kriging of spatial statistical analysis. We plot the travertine development to three types, which include excessively eroded, weakly eroded and packed. The predictive result shows that the travertine stage is a dynamic balance and a decline recombinant phase.
机译:由于喀斯特地质效应,黄龙的石灰华已经持续了数千年的十年。近年来,石灰华正在晒干,变黑,打磨,这严重影响了审美特征。我们发现,通过收集和抗真监控数据没有完善监控系统和时序数据。我们选择灰色模型,需要更少的时间数据和更高的预测结果。使用pH值因素预测石灰华开发。全黄龙预测结果基于空间统计分析的克里格。我们将石灰华开发绘制到三种类型,包括过度侵蚀,弱侵蚀和包装。预测结果表明,十字花阶段是动态平衡和重组阶段的下降。

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