| dc.creator |
ÇİMEN, Mesut |
|
| dc.date |
2017-02-28T21:00:00Z |
|
| dc.date.accessioned |
2020-10-06T10:14:28Z |
|
| dc.date.available |
2020-10-06T10:14:28Z |
|
| dc.identifier |
56955243-2b93-4a99-9e91-ed6ae32d7332 |
|
| dc.identifier |
10.1016/j.jhydrol.2016.12.056 |
|
| dc.identifier |
https://avesis.sdu.edu.tr/publication/details/56955243-2b93-4a99-9e91-ed6ae32d7332/oai |
|
| dc.identifier.uri |
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/60559 |
|
| dc.description |
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. |
|
| dc.language |
eng |
|
| dc.rights |
info:eu-repo/semantics/closedAccess |
|
| dc.title |
Comment on "Depth-discrete specific storage in fractured sedimentary rock using steady-state and transient single-hole hydraulic tests" |
|
| dc.type |
info:eu-repo/semantics/article |
|