比較分析中科虎尾園區深層水準樁、鄰近地下水位站及地陷監測井之觀測資料，

比較分析中科虎尾園區深層水準樁、鄰近地下水位站及地陷監測井之觀測資料，可瞭解虎尾地區淺層地層壓縮變化主要係隨淺層含水層影響，且淺層地層於枯水期之壓縮量在豐水期將幾近完全回復；有關建置彰化、雲林地區淺層地層壓縮連續監測系統規劃工作，其設置點位若可搭配既有地層下陷分層監測井及地下水水位觀測井，則可進一步提供釐清該設置地區之地層下陷機制之效益。

Results (English) 1:

Compared analysis in the section Huwei Park deep level pile, and near groundwater bit station and the sinkholes monitoring well of observation data, can understand Huwei area shallow layer formation compression changes main Department with shallow layer aquifer effect, and shallow layer formation Yu dry season of compression volume in Feng water period will almost completely reply; about built reset Changhua, and Yunlin area shallow layer formation compression continuous monitoring system planning work, its set points bit if can match both formation settlement layered monitoring well and the groundwater level observation well, You can further clarify the areas of subsidence mechanism of benefit.

Results (English) 2:

Comparative Analysis Branch Huwei park pile deep level, near groundwater level observation stations and land subsidence monitoring wells of information, we can understand Huwei shallow formation compressibility mainly with the impact of the shallow aquifer and the shallow strata in the amount of compression of the dry season in the wet season will almost completely reply; build about Changhua, Yunlin and shallow strata compression continuous monitoring system planning, if the set point can be layered with existing subsidence monitoring wells and groundwater level observation wells, the may further clarify the effectiveness of the formation of the set area of ​​subsidence mechanism.

Results (English) 3:

The comparative analysis of deep level pile, Huwei park adjacent groundwater station and subsidence monitoring wells of observation data, can understand the Huwei area of shallow stratum compression changes mainly with shallow aquifer, and shallow strata in the dry season of the amount of compression in the wet period will be almost completely restored; the establishment of Changhua, the Yunlin area of shallow stratum compression and continuous monitoring system planning, the set point if both collocation subsidence and groundwater monitoring well stratified water level observation well, can provide further benefits to clarify the setting of formation mechanism of subsidence area.