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Titlebook: Engineering Geology for a Habitable Earth: IAEG XIV Congress 2023 Proceedings, Chengdu, China; Volume 6: Marine and Sijing Wang,Runqiu Huan

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樓主: 萬靈藥
41#
發(fā)表于 2025-3-28 17:43:13 | 只看該作者
42#
發(fā)表于 2025-3-28 22:07:36 | 只看該作者
43#
發(fā)表于 2025-3-29 01:02:08 | 只看該作者
Dagmar Sieberichs,Hans-Joachim Krügeraquifer in Luohe formation, it shows that the groundwater recharge and runoff conditions of Anding formation and Zhiluo formation are worse, the water yield is weaker, the mineral dissolution is enhanced, the salinity in groundwater is increased, and the water quality is worse.
44#
發(fā)表于 2025-3-29 05:24:26 | 只看該作者
45#
發(fā)表于 2025-3-29 10:51:51 | 只看該作者
An Alternative Approach to Rock Mass Rating, RMR Determination from Geological Strength Index, GSI ing the formula GSI?=?RMR. – 5 for 20 limestone hills in the Ipoh area had a variance of 15%. Therefore, a modified correlation has been developed. This is GSI?=?0.889RMR. – 5 and the GSI value determined using this had a difference of only 7.6% compared to the field GSI determination. Thus, this mo
46#
發(fā)表于 2025-3-29 13:40:42 | 只看該作者
Statistics and Analysis of Compression Index of Marine Soft Soil in Lianyungang, China,relation coefficient, which is different from other regions with the highest .-. correlation coefficient. The correlation coefficient of . value with coefficient of compressibility is the highest. The fitting relationship between . with silt content and clay content is given for the first time, and
47#
發(fā)表于 2025-3-29 15:41:17 | 只看該作者
48#
發(fā)表于 2025-3-29 23:33:33 | 只看該作者
49#
發(fā)表于 2025-3-30 02:52:14 | 只看該作者
50#
發(fā)表于 2025-3-30 05:08:02 | 只看該作者
Geological Environmental Impact of Shallow Gas Release: A Case Study of Dayushan Island, East Chinater shallow gas release. The numerical simulation results are consistent with the monitoring data. The study indicates that maximum depth for shallow gas release impacts is between 32 and 65?m, and the radial impact range is within 8?m from gas release hole. The maximum soil lateral displacement is
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