摘要 |
A method of measuring a water effect on an underground non-water well includes the steps of assembling a history of water cut (WC) measurements for the well over an extended period of time, determining a water cut rate of change (R) for the well based upon the history of water cut measurements, wherein the water cut rate of change is defined as follows: <maths id="MATH-US-00001" num="00001"> <MATH OVERFLOW="SCROLL"> <MROW> <MROW> <MFRAC> <MROW> <MO>ⅆ</MO> <MROW> <MO>(</MO> <MI>WC</MI> <MO>)</MO> </MROW> </MROW> <MROW> <MO>ⅆ</MO> <MROW> <MO>(</MO> <MI>t</MI> <MO>)</MO> </MROW> </MROW> </MFRAC> <MO>=</MO> <MI>R</MI> </MROW> <MO>,</MO> </MROW> </MATH> </MATHS> and identifying whether an anomaly exists based on the determined R.
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