Comment on "Depth-discrete specific storage in fractured sedimentary rock using steady-state and transient single-hole hydraulic tests"
JOURNAL OF HYDROLOGY, cilt.546, ss.14-15, 2017 (SCI-Expanded, Scopus)
- Yayın Türü: Makale / Editöre Mektup
- Cilt numarası: 546
- Basım Tarihi: 2017
- Doi Numarası: 10.1016/j.jhydrol.2016.12.056
- Dergi Adı: JOURNAL OF HYDROLOGY
- Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
- Sayfa Sayıları: ss.14-15
- Süleyman Demirel Üniversitesi Adresli: Evet
Özet
Quinn et al. (2016) presented a method to estimate storativity (5) of fractured sedimentary rock from straddle packer tests after transmissivity (T) of aquifer was determined from low-flow constant-head (CH) step tests. Constant-rate pumping tests were carried out to determine S by using the Cooper and Jacob (1946) approximation. Estimating the aquifer parameters depends on a matching of observation data to theoretical response which is mathematically obtained from a physical model. The results of both constant rate injection and withdrawal tests in the borehole C6zone17 cannot show this simulation. This comment proposes a reasonable procedure to estimate storativity. (C) 2017 Elsevier B.V. All rights reserved.