工程地质学报
工程地質學報
공정지질학보
Journal of Engineering Geology
2015年
5期
971-975
,共5页
钻井泥浆%井液压力%失水过程%失水量
鑽井泥漿%井液壓力%失水過程%失水量
찬정니장%정액압력%실수과정%실수량
Drilling fluid%Drilling fluid pressure%Process of infiltration%Fluid loss
工程钻进过程中钻井泥浆在井液压力作用下通过孔壁泥皮失水是导致水敏性地层失稳的主要原因。为了深入了解井液失水规律,本文通过改变井液的压力差,对不同井液压力作用下钻井液漏水情况进行了模拟试验研究。实验结果表明:在相同时差内,失水量随井液压力的增大呈现先减小后增大规律;在相同井液压力下,失水的速率随时间逐渐减小,并最终趋于稳定值,失水速率的稳定值与井液压力大小没有明显的相关性;不同井液压力下,随钻井液压力的增大,前期失水量所占的比重增加;形成泥皮的质量随着井液压力的增大而增大。标准失水量随形成泥饼质量的增加呈现先减小后增大的规律。研究成果为钻井泥浆的失水特征评价、失水量的控制提供了参考依据。
工程鑽進過程中鑽井泥漿在井液壓力作用下通過孔壁泥皮失水是導緻水敏性地層失穩的主要原因。為瞭深入瞭解井液失水規律,本文通過改變井液的壓力差,對不同井液壓力作用下鑽井液漏水情況進行瞭模擬試驗研究。實驗結果錶明:在相同時差內,失水量隨井液壓力的增大呈現先減小後增大規律;在相同井液壓力下,失水的速率隨時間逐漸減小,併最終趨于穩定值,失水速率的穩定值與井液壓力大小沒有明顯的相關性;不同井液壓力下,隨鑽井液壓力的增大,前期失水量所佔的比重增加;形成泥皮的質量隨著井液壓力的增大而增大。標準失水量隨形成泥餅質量的增加呈現先減小後增大的規律。研究成果為鑽井泥漿的失水特徵評價、失水量的控製提供瞭參攷依據。
공정찬진과정중찬정니장재정액압력작용하통과공벽니피실수시도치수민성지층실은적주요원인。위료심입료해정액실수규률,본문통과개변정액적압력차,대불동정액압력작용하찬정액루수정황진행료모의시험연구。실험결과표명:재상동시차내,실수량수정액압력적증대정현선감소후증대규률;재상동정액압력하,실수적속솔수시간축점감소,병최종추우은정치,실수속솔적은정치여정액압력대소몰유명현적상관성;불동정액압력하,수찬정액압력적증대,전기실수량소점적비중증가;형성니피적질량수착정액압력적증대이증대。표준실수량수형성니병질량적증가정현선감소후증대적규률。연구성과위찬정니장적실수특정평개、실수량적공제제공료삼고의거。
The infiltration of water through wall cake pore under the effect of fluid pressure is the cause of instability of water sensitive formations during drilling process.In order to better understand the laws of infiltration, infiltration test is conducted under different fluid pressures.The test results show that when infiltration time is the same,the infiltration water increases first and then decreases with increasing of fluid pressure.When fluid pressure is the same,the infiltration rate decreases with increasing of time and eventually tends to a stable value.The stable value of infiltration rate has a low correlation with fluid pressure.When fluid pressure is different,the proportion of previous infiltration volume and the cake mass(under dry conditions)increase with increasing of fluid pressure. Infiltration of water increases first and then decreases with increasing of cake mass.The results of the test can provide reference for evaluation and control of fluid infiltration.