Epithermal Neutron Porosity Measurement
Epithermal Neutron Porosity Measurement : (adj.) Formation Evaluation. A measurement based on the slowing down of neutrons between a source and one or more detectors that measure neutrons at the epithermal level, where their energy is above that of the surrounding matter, between approximately 0. 4 and 10 eV. The slowing-down process is dominated by hydrogen, and is characterized by a slowing-down length. By measuring the neutrons at the epithermal level, rather than the thermal level, the response is a purer estimate of hydrogen index, unaffected by thermal absorbers. On the other hand, the count rate is smaller for the same source and source-detector spacing. Epithermal measurements have been made with both the compensated neutron technique and by using a pad pressed against the borehole wall with detectors focused into the formation. See: Chemical Neutron Source, Compensated Neutron Log, Excavation Effect, Hydrogen Index, Limestone Porosity Unit, Limestone-Compatible Scale, Neutron Interactions, Slowing-Down Length, Thermal Neutron Porosity Measurement
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