Cooper GBA region compromised aquitard integrity calculations

\n## **Abstract** \nThe dataset was compiled by the Geological and Bioregional Assessment Program from source data referenced within the dataset and/or metadata. Simulate the length along which a conservative solute can be transported along a fault in a period of 100 and 250 year before the concentration is less than 0.001 times the initial concentration. The calculation is based on the Grisak and Pickens (1980) equations. Create histogram of Nappamerri aquitard thickness for comparison. Full description in COO_v4_Compromised Aquitard Integrity available from https://gba-explorer.bioregionalassessments.gov.au/coo/7/34/0.\n\n\n## **Attribution** \nGeological and Bioregional Assessment Program\n\n\n## **History** \nRefer to the ipython notebook in the zip file for details of the script with the associated equation and its implementation.

## **摘要**
本数据集由地质与生物区域评估计划（Geological and Bioregional Assessment Program）基于数据集内部及/或元数据中引用的源数据汇编而成。模拟保守溶质在100年与250年时间跨度内，沿断层运移直至浓度降至初始浓度0.001倍以下时的运移长度。本次计算基于Grisak与Pickens（1980）提出的运移方程。绘制纳帕梅里弱透水层（Nappamerri aquitard）厚度的直方图以作对比分析。完整描述见《COO_v4_受损弱透水层完整性》（COO_v4_Compromised Aquitard Integrity），可通过以下链接获取：https://gba-explorer.bioregionalassessments.gov.au/coo/7/34/0。

## **归属说明**
地质与生物区域评估计划

## **编制历史**
有关关联方程及其实现脚本的详细信息，请参阅压缩包内的ipython Notebook文件。