Determining thermal rock properties of soils in Canterbury, New Zealand: Comparisons between long-term in-situ temperature profiles and divided bar measurements. (April 2018)

• Record Type: Journal Article
• Authors: Seward, Anya; Prieto, Angela
• Is Part Of: Renewable energy. Volume 118(2018)
• Page Start: 546
• Page End: 554
• Publication Date: 2018-04
• Subjects: Thermal rock properties -- Thermal diffusivity -- Ground temperature profiles -- Divided bar apparatus -- Soil; Renewable energy sources -- Periodicals; Power resources -- Periodicals; Énergies renouvelables -- Périodiques; Ressources énergétiques -- Périodiques; 333.794
• DOI: 10.1016/j.renene.2017.11.050
• Languages: English
• ISSNs: 0960-1481

Abstract

Abstract: This paper presents ground temperature data from a 9.1 m deep borehole located at Lincoln, Canterbury, New Zealand. Thermal properties of the soil are inferred from three years of in-situ temperature measurements, and compared to cored samples later measured in the laboratory using a divided bar thermal properties analysing system. The data show that seasonal changes affect ground temperatures to depths of approximately 7.5 m, beyond which the temperature is constant (±0.2°) year-round. This stable ground temperature is determined to be 11.8 °C, which is equivalent to the average ambient air temperature of the area, recorded at the adjoining weather station. Rain is seen to disturb ground temperatures immediately after the event, affecting depths up to 0.5 m by several degrees depending on the volume of water and ambient air temperature. Thermal diffusivity estimated from in-situ observation suggests soils in the top 9 m at Lincoln range from 3.4 × 10 −7 (in shallower soils) to 10.6 × 10 −7 m 2 s −1 (deeper ground). Laboratory measurements measure the diffusivity ranging from 3.8 × 10 −7 to 7.9 × 10 −7 m 2 s −1 . These values agree with the ranges measured from in situ temperature measurements. The determination of thermal properties and ground temperatures is important for the development and potential utilisation of the low enthalpy geothermal resources. Highlights: Ground temperatures are recorded in a borehole at Lincoln, Canterbury, New Zealand to a depth of 9.1 m. Constant annual ground temperatures are reached at ∼7.5 m deep with daily temperature variations reaching 0.5 m. Apparent thermal diffusivities are determined from in-situ ground temperatures over a 2- year deployment period. Thermal properties of extracted core soil samples are determined using a divided bar apparatus. Apparent thermal diffusivities are in close agreement with those values determined using the divided bar apparatus.