Skip to main content

Advertisement

Log in

2 m survey method and its improved device application in Dongshan geothermal field in Xiamen in China

  • Thematic Issue
  • Published:
Environmental Earth Sciences Aims and scope Submit manuscript

Abstract

Preliminary geothermal surveys to identify areas of potential geothermal anomalies are the most important stage in traditional hydrothermal-type geothermal resource exploration procedures. Temperature gradient wells are limited because of their accessibility issues and high costs, whereas the 2 m survey is considered a rapid, efficient, and inexpensive method to measure temperature accurately and allow for rapid vectoring toward geothermal anomalies in cases where thermal groundwater is not overlain by near-surface cold aquifers. An improved quick and portable measurement device is developed that adds in situ thermal conductivity tests based on temperature. The device, which is easy to assemble, portable, and suitable for two or three people in field work, had been calibrated by laboratory experiments. The device was applied in Dongshan geothermal field, Xiamen City in China, and 18 measurement positions were arranged. Results clearly described the geothermal anomalies in the area and revealed two temperature anomaly centers, namely a strong one in the eastern area and a weak one in the western area. Moreover, a speculated fault provided a hydraulic connection between the eastern and western areas. According to the 2 m survey, a steady-state heat conduction model has been used to inverse the 20 m temperature. The average temperature error of all boreholes in 20 m is 3 °C, whereas the relative errors between actual and forecast values are less than 10 %. Therefore, the 2 m survey method and improved device shows good performance in preliminary geothermal surveys.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 14

Similar content being viewed by others

References

  • Aretouyap Z, Nouck PN, Nouayou R (2016) A discussion of major geophysical methods used for geothermal exploration in Africa. Renew Sustain Energy Rev 58:775–781

    Article  Google Scholar 

  • Carslaw HS, Jaeger JC (1959) Conduction of heat in solids. Clarcdon Press, Oxford

    Google Scholar 

  • Cartwright K (1974) Tracing shallow groundwater system by soil temperatures. Water Resour Res 10(4):847–855

    Article  Google Scholar 

  • Coolbaugh M, Sladek C, Faulds J, Zehner R, Oppliger G (2007) Use of rapid temperature measurements at a 2-meter depth to augment deeper temperature gradient drilling. In: Thirty-second workshop on geothermal reservoir engineering

  • Elachi C (1987) Introduction to the physics and techniques of remote sensing. Wiley, New York, p 413

    Google Scholar 

  • Jia L, Guan X, Xu J (1986) An investigation into some problems of one meter thermometry in geothermal exploration. Geophys Geochem Explor 10(2):115–122

    Google Scholar 

  • Kana JD, Djongyang N, Raïdandi D et al (2015) A review of geophysical methods for geothermal exploration. Renew Sustain Energy Rev 44:87–95

    Article  Google Scholar 

  • Kappelmeyer O (1957) The use of near surface temperature measurements for discovering anomalies due to causes at depths. Geophys Prospect 5(3):239–258

    Article  Google Scholar 

  • Kratt C, Sladek C, Coolbaugh MF (2010) Boom and bust with the latest 2 m temperature surveys: Dead Horse Wells, Hawthorne Army Depot, Terraced Hills and other areas in Nevada. Geotherm Resour Counc Trans 34:567–574

    Google Scholar 

  • LeSchack LA, Lewis JE (1983) Geothermal prospecting with Shallo-Temp surveys. Geophysics 48:975–996

    Article  Google Scholar 

  • Manthena KC, Singh DN (2001) Measuring soil thermal resistivity in a geotechnical centrifuge. Int J Phys Model Geotech 1(4):29–34

    Article  Google Scholar 

  • Olmsted FH (1977) Use of temperature surveys at a depth of 1 meter in geothermal exploration in Nevada. United States Geological Survey Professional Paper, 1044-B, 25

  • Popov Y, Bayuk I, Parshin A (2012) New methods and instruments for determination of reservoir thermal properties. In: Proceedings, thirty-seventh workshop on geothermal reservoir engineering, Stanford University, Stanford, California

  • Rao MV, Singh DN (1998) Laboratory measurement of soil thermal resistivity. Geotech Eng Bull 7(3):179–199

    Google Scholar 

  • Sladek C, Coolbaugh MF, Zehner RE (2007) Development of 2-meter soil temperature probes and results of temperature survey conducted at Desert Peak, Nevada, USA. Geotherm Resour Counc Trans 31:363–368

    Google Scholar 

  • Sugawa A (1961) The distribution of the 1 m-depth ground-temperature by the various heat source. Geophys Bull Hokkaido Univ 9:21–32

    Google Scholar 

  • Thompson GEK (1964) Proceedings of United Nations Conference on New Sources of Energy, vol 2, pp 386–401

  • Trexler DT, Koenig BA, Ghusn G Jr, Flynn T, Bell EJ (1982a) Low-to-moderate-temperature geothermal resource assessment for Nevada: area specific studies, Pumpernickel Valley, Carlin and Moana. United States Department of Energy Geothermal Energy Report DOE/NV/10220-1 (DE82018598)

  • Trexler DT, Koenig BA, Flynn T, Bruce JL, Ghusn G Jr (1982b) Low-to-moderate temperature geothermal resource assessment for Nevada: area specific studies, Final Report for the Period June 1, 1980–August 30, 1981: United States Department of Energy Geothermal Energy Report DOE/NV/10039-3 (DE81030487)

  • Urakami K (1968) On a method of the underground temperature prospecting. Geophys Bull Hokkaido Univ 20:1–13

    Google Scholar 

  • Von Herzen V, Maxwell AE (1959) The measurement of thermal conductivity of deep-sea sediments by a needle-probe method. J Geophys Res 64(10):1557–1563

    Article  Google Scholar 

  • Wang J, Hu S, Pang Z et al (2012) Estimate of geothermal resources potential for hot dry rock in the continental area of China. Sci Technol Rev 30(32):25–31

    Google Scholar 

  • Yuan XZ, Li N, Zhao XY et al (2010) Study of thermal conductivity model for unsaturated unfrozen and frozen soils. Rock Soil Mech 31(9):2089–2694

    Google Scholar 

  • Zehner RE, Tullar KN, Rutledge E (2012) Effectiveness of 2-meter and geoprobe shallow temperature surveys in early stage geothermal exploration. Geotherm Resour Counc Trans 36:835–842

    Google Scholar 

  • Zhang YJ, Yu ZW, Huang R et al (2009) Measurement of thermal conductivity and temperature effect of geotechnical material. Chin J Geotech Eng 31(2):213–217

    Google Scholar 

Download references

Acknowledgments

This study was supported by the National High Technology Research and Development Program of China (863 Program) (No. 2012AA052803), the Natural Science Foundation of China (Grant No. 41372239). Some of the data set has been provided by Geological Engineering Investigation Institute of Xiamen City.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Yangyang Xie.

Additional information

This article is part of a Topical Collection in Environmental Earth Sciences on “Subsurface Energy Storage II”, guest edited by Zhonghe Pang, Yanlong Kong, Haibing Shao, and Olaf Kolditz.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Zhang, Y., Xie, Y., Zhang, T. et al. 2 m survey method and its improved device application in Dongshan geothermal field in Xiamen in China. Environ Earth Sci 75, 1290 (2016). https://doi.org/10.1007/s12665-016-6048-9

Download citation

  • Received:

  • Accepted:

  • Published:

  • DOI: https://doi.org/10.1007/s12665-016-6048-9

Keywords

Navigation