connate water

基本解釋

In contrast, connate water is the water trapped in the pores of a rock during its formation, and may be called fossil water.
相反，同生水是在巖石形成期間被圈閉在孔隙中的水，也可稱(chēng)為化石水。
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Due to the variation of geologic environment reservoir is often invaded by external water, thus, resulting in the property difference between connate water and formation water.
油藏形成后，由于地質(zhì)環(huán)境變化，儲(chǔ)層往往會(huì)受到外部水系的侵入，從而造成原生水和水層地層水性質(zhì)的差異。
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It has been proved by experiments that there's stress sensitivity in some low-permeability gas condensate reservoirs, and higher the connate water saturation, stronger the stress sensitivity.
實(shí)驗(yàn)已經(jīng)證實(shí)一些低滲深層凝析氣藏存在應(yīng)力敏感性，共生水含量越高，對(duì)壓力的敏感性越強(qiáng)。