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Ground Water Quantity Measurement on the Foot of Mt. Fuji by the Use of Radioisotopes

Journal Article · · Radioisotopes (Tokyo)
The method and results of the measurement with an improved radioisotope velocity meter, and gamma-gamma logging with radioisotopes applied to ground water investigation in Fujinomiya near Mt. Fuji are described. With the new radioisotope velocity meter, velocity and direction of ground water flow can be determined at the same time. In order to determine the depth to which the isotope velocity meter should be placed and to compare the geological column of two test borings, radioactive logging (Co60 1 mc) was made. Based on these results, it is concluded that the lava strata with medium scattering intensity are of medium porosity and have the average ground water velocity, so it was decided to put the velocity meter at 42 meters depth. The computed ground water velocity was 1.316 x 10-3 m/sec for No. 1 boring and 1.310 x 10-3/ m/ sec for No. 2 boring. Radioisotope I131 solution (0.018 mu c/ml) was used. Direction of ground water flow was determined by the dilution ratio. On the basis of the data obtained by the present measurement, the amount of the ground water which flows 1 m wide section was estimated.
Research Organization:
Agricultural Engineering Research Station, Ministry of Agriculture and Forestry
Sponsoring Organization:
USDOE
NSA Number:
NSA-17-008416
OSTI ID:
4737325
Journal Information:
Radioisotopes (Tokyo), Journal Name: Radioisotopes (Tokyo) Journal Issue: 4 Vol. 11; ISSN 0033-8303
Country of Publication:
Country unknown/Code not available
Language:
English