应用地球物理(英文版)
應用地毬物理(英文版)
응용지구물리(영문판)
APPLIED GEOPHYSICS
2005年
2期
85-88
,共4页
李斌%李子顺%朱国同%付志方
李斌%李子順%硃國同%付誌方
리빈%리자순%주국동%부지방
热传导(率)%孔隙介质%测井%油气
熱傳導(率)%孔隙介質%測井%油氣
열전도(솔)%공극개질%측정%유기
Heat-conduction rate%porous medium%logging%oil and gas evaluation
本文通过对孔隙介质中热源传热的数学物理方程分析,并结合沙桶中热源传热物理试验,发现在对储层加热过程中,油气层中点热源处的温度与水层(或干层)中点热源处的温度相比增温的速度明显地快,而在加热过程后,油气层中点热源处的温度与水层(或干层)中点热源处的温度相比降低的慢.据此提出用人工热源(炸药热源、电热源等)对地层进行加热,然后测量井中温度的动态变化,据此思想,提出了一种从孔隙介质传热出发解释油气层、预测油气产能的传热测井新方法.
本文通過對孔隙介質中熱源傳熱的數學物理方程分析,併結閤沙桶中熱源傳熱物理試驗,髮現在對儲層加熱過程中,油氣層中點熱源處的溫度與水層(或榦層)中點熱源處的溫度相比增溫的速度明顯地快,而在加熱過程後,油氣層中點熱源處的溫度與水層(或榦層)中點熱源處的溫度相比降低的慢.據此提齣用人工熱源(炸藥熱源、電熱源等)對地層進行加熱,然後測量井中溫度的動態變化,據此思想,提齣瞭一種從孔隙介質傳熱齣髮解釋油氣層、預測油氣產能的傳熱測井新方法.
본문통과대공극개질중열원전열적수학물리방정분석,병결합사통중열원전열물리시험,발현재대저층가열과정중,유기층중점열원처적온도여수층(혹간층)중점열원처적온도상비증온적속도명현지쾌,이재가열과정후,유기층중점열원처적온도여수층(혹간층)중점열원처적온도상비강저적만.거차제출용인공열원(작약열원、전열원등)대지층진행가열,연후측량정중온도적동태변화,거차사상,제출료일충종공극개질전열출발해석유기층、예측유기산능적전열측정신방법.
The results of a heat-conduction experiment with a central point source in a sand barrel shows that the temperature of the heat source increase much faster in sand saturated with oil and air (dry sand) than in water sand. During cooling the temperature of the central heat source goes down slower in oil- or air-saturated sands than in water sands. Based on the theory of heat-conduction in porous media and the experimental results, we developed a new heat-conduction logging technique which utilizes an artificial heat source (dynamite charge or electric heater) to heat up target formations in the borehole and then measure the change of temperature at a later time. Post-frac oil production is shown to be directly proportional to the size of the temperature anomaly when other reservoir parameters are fairly consistent. The method is used to evaluate potential oil production for marginal reservoirs in the FY formation in Song-Liao basin of China.