用pore water造句子，“pore water”造句

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In Changxing Basin, there are aBundant ground water resources, such as pore water of Quaternary system, fracture water of sandstone, fracture water and cavern water of carbonatite.

The strain excess pore water pressure is a response of the residual strain potential coupled with the skeleton of soil.

High variability was found in the interstitial water using a1 cm resolution device. Nitrate was never detected in the pore water.

The value of pore water pressure dissipation can be divided into two parts. One part is produced by vacuum degree and the other part by groundwater table lowering.

But the negative pore water pressure in the soft soil is smaller, which is decided by the geologic characteristics of the soft soil.

It is still deserved to study the liquefaction strength and dynamic pore water pressure and post-liquefaction character of silt when the clay particle content and silt particle content change.

The pore volumes and the amounts of pore water also may vary considerably in actively expelling source beds.

Modelling of tide induced pore water flow and solute transport in a salt marsh

Early diagenesis records and chemical composition abnormalities in pore water for methane-seep in sediments from the southern Qiongdong Basin

Change of earth pressure, pore water pressure, underground water level, surface deformation, and sub-surface movement all have direct relationship with distance between shield and testing section.

The results also showed that the relationship between the normalized pore water pressure and the generalized strain fit the bilinear model.

Although an order of magnitude smaller, the pore water pool can supply enough nutrients to build up the macrophyte biomass pool, but only if a fast turnover is attained.

Experimental research on the effect of pore water pressure on the creep laws of soft rock

The curve shape of pore water pressure developing under isotropic consolidation is not the same as that under anisotropic consolidations.

The importance to monitor the pore water pressure and to study the permeability of soil under the north anchorage of Jiangyin Yangtze River Highway Bridge is analyzed firstly.

The conclusion shows that DJM has more influence on the pore water pressure of the upper soil, and PVD and DJM both have more influence on the lower soil.

Use of on-site burial of pore water pressure meter, to pore water pressure dissipation over the situation to determine the number of tamping, tamping the time interval between times.

The effect of different cyclic shear stress path under isotropic consolidation on the relationship of pore water pressure and accumulated energy dissipation is very little, itcan be ignored.

Water filling sources of underground mine in Pingshuo mining area have Quaternary pore water, surface water, Permo-Carboniferous sandstone fissure water and Ordovician limestone karstic fissure water.

Based on the analysis and research on test results, it discusses the existence of low water-cut oil layers due to porous media and pore water in micro pores of reservoir.

The soil samples used in the test are under half-solid state in which the bound water is principal part of pore water.