摘要
郭庄泉为一全排型、侵蚀—构造上升泉,出露于中奥陶纪灰岩中。对泉流量及降水量进行了谱分析,泉流量周期为8.5年、25个月及12个月等,泉的年内滞后期为6—7个月、经回归分析和滑动平均模型计算,当年的泉流量与自前一年起的11年内的降水量关系密切。
The Guozhuang Spring exposed in the Middle Ordovician limestone is one of complete-drainage and of erosion structure of ascending type. In the light of the spectral analysis of the spring discharge and precipitation, the cycles of the spring discharge are 8.5 years, 25 months and 12 months and the lag time is 6—7 months. The spring discharge is closely correlated with the precipitation within a period of 11 years ago from the previous year on by the analysis of regression and the calculation of moving average model.
出处
《中国岩溶》
CAS
CSCD
北大核心
1989年第3期242-248,共7页
Carsologica Sinica
