痛打
发表于 2025-3-26 23:31:00
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fetter
发表于 2025-3-27 01:08:32
Advances in understanding the relation between reservoir properties and facies distribution in the Pporosity and permeability up to 1 D. Bioturbation leads to pronounced anisotropy in some horizons. Of major importance, however, are late diagenetic cementation effects which focus on faults, fractures and horizontal to subhorizontal discontinuities. Most widespread is iron cementation which makes u
合并
发表于 2025-3-27 07:13:20
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千篇一律
发表于 2025-3-27 10:31:47
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小虫
发表于 2025-3-27 15:18:54
First outcomes from groundwater recharge estimation in evaporate aquifer in Greece with the use of Asible to corroborate the validity of the method in this phase of the research. In the frame of a research project taken place in the study area, discharge values are measured at the springs draining the system; thus the validation of the method will be done in the next step of this study.
Tractable
发表于 2025-3-27 21:14:10
Adumbration of Amvrakia’s spring water pathways, based on detailed geophysical data (Kastraki - Meteographic corrections, as the area had not smooth relief. Five (5) VLF profiles were conducted with different directions around the spring’s area, in order to detect possible conductive zones in the conglomerates surrounding the study area. Moreover, two (2) ERT sections of a total length of 140m wer
和平
发表于 2025-3-28 00:34:07
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Blatant
发表于 2025-3-28 04:14:29
Gurpreet Sodhi MD,Ramesh Singh MDication of the conductible fracture in the aquifer has thus received growing interest over the past decades. This paper summarizes the major findings from the first year of a hydrogeological investigation program initiated by the Central Geological Survey, Ministry of Economic Affairs (MOEA) of Taiw
intercede
发表于 2025-3-28 09:27:47
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esoteric
发表于 2025-3-28 13:53:47
Linda Bogar,April Stempien-Oteroer aquifers in the study area, Vertical Electrical Sounding (VES) were carried out at 25 locations; five each on a 100m long traverse and 1-D inversion of the VES data with pseudo 2-D presentation was carried out. The inverted resistivity models were calibrated with borehole data in the vicinity of