巖心(xin)驅替(ti)可(ke)視化系(xi)統(tong)
隨著(zhe)水驅開發(fa)的進(jin)行(xing),國(guo)內大(da)多數油田(tian)皆(jie)已進(jin)入(ru)高(gao)含水、高(gao)采出(chu)程(cheng)度的“雙高(gao)"階段,針(zhen)對二次采油(you)未(wei)能采出(chu)的未波(bo)及(ji)區的剩(sheng)余油(you)和波(bo)及(ji)區的殘余油,認(ren)識剩(sheng)余油(you)為油(you)田(tian)二(er)次采油(you)及(ji)三(san)次采油(you)提供重(zhong)要(yao)依(yi)據尤為重(zhong)要(yao)。

剩(sheng)余油(you)分布是(shi)指剩(sheng)余油(you)在地層(ceng)中的分布情(qing)況,影(ying)響剩(sheng)余油(you)分布的因(yin)素眾(zhong)多,主(zhu)要(yao)受(shou)靜(jing)態儲(chu)層(地質(zhi)的)和動(dong)態(tai)註(zhu)采(cai)狀(zhuang)況(kuang)(開(kai)發(fa)的)雙重(zhong)因(yin)素的影響。靜(jing)態儲(chu)層因(yin)素是(shi)根本的、內在的因(yin)素,註(zhu)采狀(zhuang)況(kuang)(開(kai)發(fa)條(tiao)件(jian))是(shi)影(ying)響剩(sheng)余油(you)分布的外部因(yin)素。
巖心(xin)驅替(ti)核(he)磁共振原理
基於核(he)磁對氫(qing)信(xin)號優秀的捕捉(zhuo)能力,在油(you)氣(qi)藏(zang)儲(chu)層研(yan)究(jiu)中(zhong),發(fa)揮(hui)了巨大(da)的作用(yong)。搭配(pei)多場(chang)耦合(he)配件,可(ke)以(yi)模(mo)擬(ni)地層(ceng)真實(shi)高(gao)溫高(gao)壓(ya)環境(jing),巖心(xin)(水驅油核(he)磁共振實(shi)驗、水驅剩(sheng)余油(you)分布實(shi)驗、微(wei)觀驅替(ti)實(shi)驗、多相(xiang)驅(qu)替(ti)實(shi)驗)不同(tong)尺(chi)寸(cun)孔隙中(zhong)的油水信號在核(he)磁T2譜中(zhong)對應(ying)的弛(chi)豫(yu)時間(jian)不同(tong),隨著(zhe)驅(qu)替(ti)實(shi)驗(水驅油核(he)磁共振實(shi)驗、水驅剩(sheng)余油(you)分布實(shi)驗、微(wei)觀驅替(ti)實(shi)驗、多相(xiang)驅(qu)替(ti)實(shi)驗)的進(jin)行(xing),核(he)磁T2譜隨著(zhe)巖心(xin)內部(bu)油水相態(多相(xiang)驅(qu)替(ti))的變(bian)化而(er)發(fa)生變(bian)化,可(ke)以(yi)用(yong)定(ding)量(liang)來研(yan)究(jiu)地層(ceng)的油氣開采(cai)過程(cheng)。同時基於(yu)核磁成像(xiang)功(gong)能,可(ke)以(yi)實(shi)現(xian)對整個(ge)驅(qu)替(ti)過(guo)程(cheng)(水驅油核(he)磁共振實(shi)驗、水驅剩(sheng)余油(you)分布實(shi)驗、微(wei)觀驅替(ti)實(shi)驗、多相(xiang)驅(qu)替(ti)實(shi)驗)的各個(ge)階段進(jin)行(xing)成像(xiang),生動(dong)形象(xiang)的觀察(cha)動(dong)態(tai)變(bian)化。實(shi)現(xian)驅(qu)替(ti)過(guo)程(cheng)(水驅油核(he)磁共振實(shi)驗、水驅剩(sheng)余油(you)分布實(shi)驗、微(wei)觀驅替(ti)實(shi)驗、多相(xiang)驅(qu)替(ti)實(shi)驗)中(zhong)油水變(bian)化的可(ke)視化。

巖心(xin)驅替(ti)可(ke)視化系(xi)統(tong)框架(jia)圖(tu)
巖心(xin)驅替(ti)可(ke)視化系(xi)統(tong)
MacroMR高(gao)溫高(gao)壓(ya)巖心(xin)驅替(ti)可(ke)視化系(xi)統(tong)能夠結(jie)合(he)傳統的外圍驅(qu)替(ti)系(xi)統(tong),實(shi)現(xian)模(mo)擬(ni)地層(ceng)高(gao)溫高(gao)壓(ya)環境(jing),對巖心(xin)進(jin)行(xing)全(quan)過程可(ke)視化驅(qu)替(ti)研(yan)究(jiu),可(ke)視化可(ke)以(yi)定(ding)性(xing)的評(ping)價(jia)巖心(xin)驅替(ti)情(qing)況,通過(guo)譜(pu)圖(tu)變(bian)化可(ke)定(ding)量(liang)計(ji)算出(chu)驅(qu)替(ti)量(liang)的多少;可(ke)以(yi)任意(yi)層面、多角(jiao)度對巖心(xin)進(jin)行(xing)無(wu)損(sun)切(qie)片(pian)選層(ceng)觀測(ce)和(he)分(fen)析;

巖心(xin)驅替(ti)可(ke)視化系(xi)統(tong)


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