The present invention provides a down hole
spectrometer for determination of
dew point pressure to determine an associated optimal pumping rate during sampling to avoid
precipitation of asphaltenes in a formation sample. A sample is captured at formation pressure in a controlled volume. The pressure in the controlled volume is reduced. Initially the
formation fluid sample appears dark and allows less
light energy to pass through a sample under test. The sample under test, however, becomes lighter and allows more
light energy to pass through the sample as the pressure is reduced and the
formation fluid sample becomes thinner or less dense under the reduced pressure. At the
dew point pressure, however, the sample begins to darken and allows less
light energy to pass through it as apshaltenes begin to precipitate out of the sample. Thus, the
dew point is that pressure at which peak light energy passes through the sample. The
dew point pressure is plugged into an equation to determine the optimum pumping rate for a known mobility, during sampling to avoid dropping the pressure down to the
dew point pressure to avoid
asphaltene precipitation or dew forming in the sample. The
bubble point can be plugged into an equation to determine the optimum pumping rate for a known mobility, during sampling to avoid dropping the pressure down to the
bubble point pressure to avoid bubbles forming in the sample.