石油化工高等学校学报
石油化工高等學校學報
석유화공고등학교학보
JOURNAL OF PETROCHEMICAL UNIVERSITIES
2014年
5期
50-53
,共4页
郭龙江%李威%秦国顺%吉树鹏%李树军%杨肖曦
郭龍江%李威%秦國順%吉樹鵬%李樹軍%楊肖晞
곽룡강%리위%진국순%길수붕%리수군%양초희
气井%碳酸钙结垢%原因分析%结垢趋势预测
氣井%碳痠鈣結垢%原因分析%結垢趨勢預測
기정%탄산개결구%원인분석%결구추세예측
Gas well%Calcium carbonate scale%Cause analysis%Prediction of scaling tendency
针对松南气田气井井筒结垢问题,对垢进行成分分析,并在室内条件下进行结垢实验研究,同时利用饱和指数法对气井结垢进行结垢趋势预测研究。结果表明,松南气井井筒垢物主要为碳酸钙,在一定的井筒产出水中,其他条件不变的情况下,结垢质量随温度的升高而增大,随压力的升高而减小。结合压井液和地层水的配伍性实验可以得出:结垢的主要原因是CaCl2型压井液与地层水的不配伍性,地层水进入井筒后压力下降导致 CaCO3溶解度下降产生沉淀结垢;利用 Oddo-Tomoson饱和指数法对CaCO3结垢趋势的理论预测结果与实际测量结果一致。
針對鬆南氣田氣井井筒結垢問題,對垢進行成分分析,併在室內條件下進行結垢實驗研究,同時利用飽和指數法對氣井結垢進行結垢趨勢預測研究。結果錶明,鬆南氣井井筒垢物主要為碳痠鈣,在一定的井筒產齣水中,其他條件不變的情況下,結垢質量隨溫度的升高而增大,隨壓力的升高而減小。結閤壓井液和地層水的配伍性實驗可以得齣:結垢的主要原因是CaCl2型壓井液與地層水的不配伍性,地層水進入井筒後壓力下降導緻 CaCO3溶解度下降產生沉澱結垢;利用 Oddo-Tomoson飽和指數法對CaCO3結垢趨勢的理論預測結果與實際測量結果一緻。
침대송남기전기정정통결구문제,대구진행성분분석,병재실내조건하진행결구실험연구,동시이용포화지수법대기정결구진행결구추세예측연구。결과표명,송남기정정통구물주요위탄산개,재일정적정통산출수중,기타조건불변적정황하,결구질량수온도적승고이증대,수압력적승고이감소。결합압정액화지층수적배오성실험가이득출:결구적주요원인시CaCl2형압정액여지층수적불배오성,지층수진입정통후압력하강도치 CaCO3용해도하강산생침정결구;이용 Oddo-Tomoson포화지수법대CaCO3결구추세적이론예측결과여실제측량결과일치。
For the problem of scaling in producing wells in Songnan gas fields,components of the scale samples were analyzed for its,and scaling experimental research was done indoor.In addition,the trend of scaling in gas wells was predict using saturated index method.Results showed that the scale in Songnan gas wells was mainly calcium carbonate.When the well producing water was fixed,the scaling quantity arised with the temperature increasing,while reduced with the pressure rising. Considering the compatibility test,it was indicted that the mainly scaling reason was the mismatch between the CaCO3 well killing fluid and the stratum water,which caused the decrease of pressure when the stratum water get into the wellbore. Theoretic prediction on the tendency of the scaling of CaCO3 was made with the Oddo-Tomoson saturating exponential method, and the result was consistent with the measurement in field.