The development of ground source heat pumps has facilitated the use of geothermal power at shallow depths. Soil thermal diffusivity is a crucial physical parameter that affects soil temperature. This study provides an algorithm to estimate soil thermal diffusivity at any water content from data on soil texture, bulk density, and percentage of organic carbon. Previous studies have proposed methods to estimate thermal parameters.
Soil thermal diffusivity values have been calculated at 56 sites using temperature data from uk met office weather stations. Estimating thermal properties for this zone is difficult as it is heterogeneous and is subject to seasonal water content variations. Indirect estimation of soil thermal properties and water. Estimating apparent thermal diffusivity of soil using field temperature time series article in geomechanics and geoengineering 111. An empirical model for estimating soil thermal diffusivity from texture, bulk density, and degree of saturation xiaoting xie,yili lu, and tusheng ren college of resources and environmental sciences, china agricultural university, beijing, china. Pedotransfer functions ptfs are widely used for estimating soil thermal diffusivity. In heat transfer analysis, thermal diffusivity is the thermal conductivity divided by density and specific heat capacity at. Results of soil thermal conductivity and borehole resistance estimates from three in situ tests. We aimed to determine soil thermal diffusivity from halfhourly temperature measurements in a. Hydraulic tomography for estimating the diffusivity of. Models were trained on the dataset of 77 soil samples including silty clays, silty clay loams, silt loams, clay loams, loams, sandy clay loams, sandy loams, loamy sands, and sands. Insulation bidding software insulation companies everywhere can breathe a sigh of relief once they start using ensigns easytouse insulation estimating software, designed specifically to. Priority academic program development of jiangsu higher.
A new method to determine the thermal properties of soil. Estimating soil thermal diffusivity with interference. Soil temperature variations with time and depth model. Request pdf estimating soil thermal diffusivity with interference analyses the development of ground source heat pumps has facilitated the use of geothermal power at shallow depths. To accurately determine your soils thermal diffusivity, we need to know what your soil conditions are, including the types of soil clay, sand, gravel, silt, top soil, and many others, and the. Soil thermal diffusivity from soil composition and particle arrangement according to the semiempirical model proposed by farouki 1986 with f s and f a representing the ratios of average. Hydraulic tomography for estimating the diffusivity of heterogeneous aquifers based on groundwater response to tidal fluctuation in an artificial.
The modeling of soil temperature in time and depth requires knowledge of the soil surface energy balance and of soil thermal properties. The amount of information yielded by thermal analysis measurements is even greater with the wide selection of specialized advanced software. Analysis of thermal diffusivity data determined for selected organic topsoil layer. A transient method was used to measure the thermal diffusivity of a fine sand. Estimating apparent thermal diffusivity of soil using. Six prevalent algorithms to calculate soil thermal diffusivity are. Introduction 2 in the past decade, soil thermal research has advanced development of the heat pulse technique for estimation of soil thermal properties, i.
Estimating soil heat flux using distributed temperature sensing 143 the soil heat flux calculated from the temperatures of the upper and middle cable does not directly reflect the surface heat. Estimating soil thermal diffusivity using pedotransfer functions. These properties influence how energy is partitioned. Initially, ground heat exchangers were buried in trenches. Reliable estimates of soil thermal properties such as heat capacity, thermal conductivity, and diffusivity are important in analysis of heat transmission through soils in applications such as shallow geothermal applications, buried electrical conduits, and in general heatfluid flow analyses. Determining soil moisture and soil properties in vegetated. In a conductive system, the thermal diffusivity is a func daily cycles of temperature at increasing depths. Information on soil thermal properties is needed for estimating soil temperature t and heat flux. Error analysis in estimating temperaturedependent thermal.
Soil profile method for soil thermal diffusivity, conductivity and heat. Pdf estimation of thermal diffusivity for greenhouse soil. The soil heat flux g is a key parameter for closing energy balance, and a significant variable to understand the surface processes, principally in meteorological applications. Analysis of thermal diffusivity data determined for. Pdf estimation of thermal diffusivity of soils in antarctica using. The change in heat storage is based on the soil temperature change in the layer over the time period and an estimate of the soil thermal heat capacity that is. One alternative capable of estimating both thermal properties. The aim of the work was to validate usage ptfs with nonlinear regression nlr for estimating soil thermal diffusivity kd, moreover was to select the best predictor variables used for. The empirical parameters b1, b2, and b3 depend on soil physical properties. Soil thermal diffusivity estimated from data of soil temperature and. Tests were conducted for three bulk densities and seven volumetric water contents. Soil thermal diffusivity and water transport in unsaturated, nonisothermal, salty soil ibrahim nassar nassar. Standard test method for calculating thermal diffusivity. Their system determined soil thermal diffusivity and calculated thermal.
Program through the national research foundation of korea nrf. Estimating seasonal values of thermal diffusivity in. Thermal diffusivity calculator solving for thermal diffusivity given thermal conductivity, density and specific heat capacity. It can be calculated from thermal conductivity and volumetric heat capacity. A numerical model to estimate the soil thermal conductivity. Simulated responses of permafrost distribution to climate. Thermal conductivity for a gravelly soil measured in situ was appreciably lower than that of the sieved and homogeneous laboratory soil columns.
Thermal diffusivity k t is a very complex soil property. Estimating soil heat flux using distributed temperature. Comparison of six algorithms to determine the soil thermal diffusivity. Thermal conductivity and diffusivity estimations for. Some attempts have been made to indirectly predict soil thermal diffusivity from the easy available fundamental soil physics properties. Simulated responses of permafrost distribution to climate change on the qinghaitibet plateau. Estimating soil thermal diffusivity at different water. The thermal diffusivity of various soil layers for the first three harmonics have been calculated using amplitudes and phase angles of the soil temperature wave. Thus, there are two objectives in estimating soil thermal diffusivity. Estimating soil thermal diffusivity at different water contents from easily available data on soil texture, bulk density, and organic carbon content. Soil thermal diffusivity estimated from data of soil. The thermal properties of soil are a component of soil physics that has found important uses in engineering, climatology and agriculture. An empirical model for estimating soil thermal diffusivity.
Thermal conductivity, thermal diffusivity, density, and specific heat may be calculated by selection of. Thermal diffusivity equations calculator aj design software. Estimating soil thermal diffusivity using pedotransfer. Junichi uno and kanichi hayakawa, a method for estimating thermal diffusivity of heat conduction food in a cylindrical can, journal of food science, 45, 692695 1980 10.
210 937 1600 467 610 421 821 4 876 1437 16 292 716 199 275 1344 600 1583 165 1095 1106 642 1469 1251 111 52 1401 1503 805 823 60 517 653 392 848 1206 1469 586 65 1151 1243 1251 266 1160 1112 1449 893