A method for determining the replenishment source of karst springs
A method for determining the source and the technology for replenishing the source, which is applied in the field of determining the source of the karst big spring to achieve the effect of easy data, simple method and strong practicability.
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specific Embodiment approach
[0098] As a specific implementation, this embodiment selects the data on June 14, 2016 (the lowest day of the spring water level in this year) to draw the contour map of the karst groundwater level in the dry season, and draws the data on August 22, 2016 (the highest day of the spring water level in the current year). The contour map of the karst groundwater level in the wet season; select the data on April 21, 2018 (the lowest day of the spring water level in this year) to draw the contour map of the karst groundwater level in the dry season, and the data on September 3, 2018 (the day of the highest spring water level in the current year) Draw the contour map of the karst groundwater level in the wet period. After comparative analysis, the confluence trend reflected by the four contour maps is consistent, so the contour map drawn based on the data on September 3, 2018 is selected as the map of the confluence trend of groundwater to the karst spring, as shown in image 3 shown...
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