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Continuous Temperature Logging in Air across the Deep Vadose Zone

Marshall Reiter*

New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801


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Fig. 1. Sensor assembly showing electrical connection and sensor assembly attached to cable with stainless-steel protection hoop. Black tip at the end of the glass bead is the thermistor enclosed in a thin watertight glass layer. The scale applies only to the upper probe; the lower probe is an enlargement.

 


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Fig. 2. Temperature vs. depth data, temperature logs, for six different days. Dates logged (month, day, year) and logging speed are given in legend. Logs are offset 0.5°C so they can be compared.

 


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Fig. 3. Temperature vs. depth data from the 1- to 10-m depth for six different logs. Dates logged (month, day, year) and logging speed are given in legend.

 


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Fig. 4. Daily highs and lows in Albuquerque about 35 km north of the Tome site. Dates of temperature logs are indicated, beginning with 5.26 (month, day).

 


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Fig. 5. Temperature difference between Log 3 and other logs, and between Logs 5 and 6, below 10 m.

 


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Fig. 6. Temperature gradients for Logs 3, 5, and 6 starting at the 5-m depth. Note log scale for low gradient enhancement.

 


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Fig. 7. Temperature gradients for Logs 1, 2, and 4; note log scale for low gradient enhancement.

 





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