pore space

基本解釋

The pore space preserves the shape, or mold, of the dissolved material.
孔隙空間保留著被溶解的物質(zhì)形狀或印模。
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The porosity increasing is primarily due to the resolution of carbonate so that a large amount of the secondary pore space is resulted.
而碳酸鹽的溶解作用形成了大量次生孔隙空間，增加了砂巖的孔隙度。
In the original conditions, reservoir rocks and fluids inside the pore space in the pressure equilibrium, once the oil drilling, this balance was destroyed.
在原始條件下，油層巖石與孔隙空間內(nèi)的流體處于壓力平衡狀態(tài)，一旦鉆開油層，這種平衡就被破壞。

孔隙
The objective of this thesis is to use a combination of numerical modeling and experiments to investigate the fundamentals of solute transport in pore space of soil with a view to improve modeling at macroscopic scales, which can be used to investigate the movement of nutrients under drip fertigation.
本文采用理論模擬和室內(nèi)外試驗(yàn)研究相結(jié)合的方法，重點(diǎn)研究了溶質(zhì)在土壤孔隙運(yùn)動(dòng)的微觀機(jī)理，提出了改進(jìn)的溶質(zhì)運(yùn)移模擬模型，在此基礎(chǔ)上模擬了不同溶質(zhì)在土壤中的運(yùn)移，并通過室內(nèi)滴灌條件下水氮分布試驗(yàn)，應(yīng)用上述模型模擬了滴灌條件下水分及氮素運(yùn)移。
地球科學(xué)
孔腔
孔洞