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Establishment of a Groundwater Management Index for the Szuchung Creek Hot-Spring

机译:建立斯春河温泉的地下水管理指数

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In the establishment of the groundwater management index of the Szuchung Hot-Spring Area, the sensitivity of the temperature change is much smaller than the sensitivity of the groundwater level change. Therefore, only the groundwater level can be used as the management index. According to the records of existing hot spring observations, the groundwater level of each observation well has changed significantly during the short period of time due to the influence of artificial utilization, and overall it is still affected by the abundance and dry season. In order to obtain a standard management basis, it is necessary to calculate the overall groundwater level change baseline first to deducte the human influence. But lacking the long-term development record of the measured hot spring well, so it can only use the existing data for data analysis. In order to obtain the threshold value of management indicators, thisstudy uses the mobile average and geometric average of Dashan Old Station and Public Bathroom Station to obtain the benchmark groundwater level of each station. Then, with the standard deviation of one standard deviation, two standard deviations, and the largest drop in history, the actual groundwater level, safe groundwater level, severe groundwater level, and bottom limit groundwater level can be obtained. After the comparison, it was learned that Dashan Old Station recorded the lower than the bottom limit groundwater level in about three days in March and April 2016, and the number of days was lower than the safe groundwater level. The actual groundwater level of the Public Bathroom Station was almost above the safe groundwater level.
机译:在建立Szuchung热弹簧区域的地下水管理指标时,温度变化的灵敏度远小于地下水位变化的灵敏度。因此,只有地下水位可以用作管理指标。根据现有热弹簧观测的记录,由于人工利用率的影响,每次观察井的地下水位在短时间内发生了显着变化,并且整体仍然受到丰富和干燥季节的影响。为了获得标准管理的基础,有必要首先计算整个地下水位变化基线以扣除人类影响力。但缺乏测量温泉的长期发展记录,因此它只能使用现有数据进行数据分析。为了获得管理指标的阈值,鉴定使用大山旧站和公共浴室站的移动平均和几何平均值,以获得每个站的基准地下水位。然后,随着一个标准偏差的标准偏差,两个标准偏差,以及历史上最大的下降,实际地下水位,安全地下水位,严重的地下水位和底部极限地下水位。比较后,据了解,大山旧站在3月和2016年4月在大约三天内记录了低于底部限制地下水位,并且数天数低于安全地下水位。公共浴室站的实际地下水位几乎高于安全地下水位。

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