At the first stage of buried dissolution,the acidulous water enriched organic acid with strong dissolution causes the formation of intragranular dissolved pore,intergranular dissolved pore,intercrystalline dissolved pore and cave etc.

第1期埋藏溶蝕與富含有機酸的酸性水有關(guān)且溶蝕強烈，形成大量的粒內(nèi)溶孔、粒間溶孔干少妇33P图、晶間溶孔和溶洞等次生孔隙国产一级一区真人无码播放视频。

By using Lee\'s matching law, the excess pore-air pressure, excess pore-water pressure and settlement in the Laplace-transformed domain are obtained for one-dimensional consolidation in unsaturated soils, under the large-area uniform instantaneous loading. A computer program using the method by Crump and Durbin is developed to obtain the semi-analytical solution of the excess pore-air pressure, excess pore-water pressure and settlement under the boundary conditions of the top surface permeable to water and air and the bottom impermeable to water and air.

8采用李氏比擬法，應(yīng)用Merchant粘彈性模型美女视频网址，得到了Laplace變換域內(nèi)粘彈性非飽和土地基一維固結(jié)時超孔隙水壓力，超孔隙氣壓力以及土層沉降的解丁香花色色网；采用Crump及Durbin方法實現(xiàn)Laplace逆變換色一鲁中文字幕，獲得大面積均布瞬時加荷，在頂面排氣排水真人av在线免费看，底面不排氣不排水情況下粘彈性非飽和土地基一維固結(jié)時的半解析解中国无毛黄色视频。

The pore capacity is becoming smaller with increasingthe vitrinite content. 2. Micro-porosity is dominated in the total pore capacity, which takes more than50%. There is not relationship among pore capacity and specific surface with otherfactors such as Maceral and R0, which shows that the distribution and shapes of poreare not influenced by the composition of the coal. 3. The pore is opened for the coal of Ordos Basin, the order is from durain to clarainthen samples to vitrain. Others are belong to half-opened and thin throat. 4. The adsorption content of gas is increasing with the higher pressure, and the freegas content is decreasing;The adsorption content of gas is decreasing with thehigher temp, and the free gas content is increasing;The adsorption content of gas isincreasing with higher vitrinite content for the kennel coal when temp.

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By field-testing methods, such as static cone penetration test, field vane shear test, and pore water piezometer test, the variation of strength and the pore water pressure are measured at real time, and the marine hydrodynamics' impaction on the consolidation process of the sediments in the Yellow River Estuary was studied. It is shown that the self-consolidated sediments have a very fast consolidation rate, under self-consolidation, in 72h, the consolidation degree reaches 37% and about 142h the pore water pressure disperse over, while under the hydrodynamics, in 72h the consolidation degree reaches 52% and about 195h the pore water pressure disperse over.

在黃河三角洲刁口葉瓣潮坪上，開挖2m×1m×1m的試坑不卡无码av一区二区丝袜，現(xiàn)場取土配置黃河口快速沉積形成的流體狀堆積物激情文学欧美图片乱伦，以鐵板部分覆蓋試坑隔絕波浪和潮流作用，利用微型貫入在线视频亚洲日韩、靜力觸探午夜欧美福利视频、十字板剪切試驗、孔隙水壓力監(jiān)測等原位測試手段国产成年精品,免费视频大全，實時測定快速沉積的海床土強度發(fā)展以及孔隙水壓力消散情況99在线视频播放，研究快速沉積的粉質(zhì)海床土分別在自重條件下以及在波浪和潮波等水動力作用下的固結(jié)過程。

The pore distribution in the direction of coating thickness was self-existent and could not join to intercommunicating pore.The pore diameter was very tiny so that it could prevent hydrotropic solution entering into the pore.

機械鍍鋅的形層過程既沒有熱鍍鋅那樣的高溫冶金反應(yīng)日本最新免费二区三区，也沒有電鍍鋅那樣的電沉積效應(yīng)亚洲欧美有码中文字幕，鍍層是常溫常壓下利用化學吸附沉積和機械碰撞使金屬鋅粉在工件表面鑲嵌堆積而成[1]又黄又湿的网站，所以人們認為機械鍍鋅鍍層的致密性要低于電鍍和熱鍍鋅鍍層，但機械鍍鋅鍍層又表現(xiàn)出良好的耐腐蝕性能午夜黄色网站免费成年人。

Ca2 was activated by microwave to investigate its physical characteristics and dechloriantion.The change of total pore area,pore area of different pore size zone,pore size distribution of the sample before and after reaction of different microwave activation was examined by mercury porosimeter.

采用微波爐對一定質(zhì)量的氫氧化鈣樣品進行活化av网站在线免费，利用壓汞儀考察了不同微波活化時間及脫氯反應(yīng)前后的Ca2總比孔表面積、分段比表面積和孔徑分布的變化色秀视频久久久，并在脫氯實驗臺上對脫氯效率進行實際測試影音先锋图片资源专区。

The Changxing Formation reservoirs are mainly a set of reef dolomite, sparry oolitic dolomite, and have moderate to high porosity, moderate to high permeability and good physical properties. The reservoir space types are mainly intercrystalline pore, intercrystalline solution pore, intergranular dissolved pore, intragranular dissolved pore, moldic pore and dissolved expanding pore, and to a lesser extent, crack and suture.

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According to permeability, associating with pore type, pore throat radium, ratio of pore throat radium, and connectivity of pore throat, the reservoir is divided into two groups: moderate permeability reservoir with moderate pore and small throat and low permeability reservoir. the latter is further classified into three types: moderate pore and small throat reservoir, small pore and unhomogeneous and subtle throat reservoir, and small pore and homogeneous and subtle throat reservoir.

在此基礎(chǔ)上狠狠操人人操人人干，以滲透率為主線日欧美老女人，結(jié)合孔隙類型、孔喉半徑人人操人人看人人搞、孔喉半徑比以及孔喉連通性等參數(shù)真人版AV黄色网站，將研究區(qū)儲層主要劃分為中滲透儲層和低滲透儲層2種基本類型，前者以中滲透中孔細喉道型為主国产黄色在线观看q，后者又進一步細分為低滲透中孔細喉道型大黄色一级片、低滲透小孔不均勻微細喉道型和低滲透小孔較均勻微細喉道型等3個亞類。

Under the microenvironments of fruit bagging,Alternaria had always been the major fungi in different bags,sites of fruit and weather conditions during the whole growing season. As the secondary major fungi,Penicillium had always been after July and emerged later in inner bag and cortical pore than other sites.In the bag with which the inner bag was red and waxing,Trichoderma was isolated first in pericarp without cortical pore and inner bag as well as later in cortical pore after August.In \'Kobayashi\' bag which inner bag was red and waxing, Aspergillus and Fusarium were isolated in pericarp without cortical pore and cortical pore after bag removed.Alternaria and Penicillium were isolated in unbagging fruit and \'Qianwei\' bag which inner bag was red and unwaxing and the date Penicillium was isolated in CK was 45d later than bagging treatment.Under high temperature weather condition,there were no differences in the fungi population structure on fruit surface among all treatments.And the fungi population structure on fruit surface in bagging apple was more than that of unbagging ones under overcast and rainy condition.

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And (2) the pore pressure is mainly controlled by volumetric strain. Stress can directly make the pore volume change, and indirectly control the variation of pore pressure changed by the pore volume.

2巖石孔隙內(nèi)流體壓力的變化主要受體積應(yīng)變控制，應(yīng)力的直接作用是使巖石孔隙體積發(fā)生非線性變化鲁鲁鲁www，對流體壓力變化的影響是通過巖石孔隙體積變化實現(xiàn)的人人干人人操人人草人人摸，是間接的。