Access the full text.
Sign up today, get DeepDyve free for 14 days.
K. Adamowski, T. Hamory (1983)
A stochastic systems model of groundwater level fluctuations.Journal of Hydrology, 62
G. Huthmann, K. Wilke (1982)
Time and frequency domain analyses of hydrological systemsJournal of Hydrology, 55
Abstract The fluctuation of most of the hydrograph in the deep aqueous system records the fluid pulsation in lithosphere and variation of the earth's crust. Many observations have verified that groundwater is an ideal information carrier of the crust. In this paper, the series of input (precipitation, air pressure, Earth tide etc.) and output (water level, artesian flow) of the deep aqueous system are studied by using the spectrum analysis and system theory. The application concepts of transfer function and the spectral structure of the hydrograph enrich the knowledge of the deep aqueous system. Two typical spectral structures of the hydrograph of the deep aqueous system are obtained by comparing with many water—bearing systems of the Jizhong depression. One is from well Ma—17 and the other is from the well Xinze—5. Finally, the physical models of forming the spectrum of the hydrograph are constructed on the basis of the spectrum research on the deep aqueous system.
Acta Geologica Sinica (English Edition) – Wiley
Published: Dec 1, 1993
Keywords: ; ;
Read and print from thousands of top scholarly journals.
Already have an account? Log in
Bookmark this article. You can see your Bookmarks on your DeepDyve Library.
To save an article, log in first, or sign up for a DeepDyve account if you don’t already have one.
Copy and paste the desired citation format or use the link below to download a file formatted for EndNote
Access the full text.
Sign up today, get DeepDyve free for 14 days.
All DeepDyve websites use cookies to improve your online experience. They were placed on your computer when you launched this website. You can change your cookie settings through your browser.