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Soil Temperature Regime at Ahmedabad [PDF]
A 3-m deep probe with five PT 100 temperature sensors was installed at the campus of Indian Institute of Management, Ahmedabad in August, 1999 to monitor temperature at various depths. Hourly values from all the sensors were noted one day in each month for a year.
Sharan, Girja, Jadhav, R.
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Effect of Groundwater Level on Soil Moisture, Soil Temperature and Surface Temperature
Journal of the Indian Society of Remote Sensing, 2021The dynamic behavior of groundwater level effects the soil moisture, soil temperature and surface temperature. In the study, the effect has been studied at two observation sites with varying groundwater level. Regular measurements of soil moisture and soil temperature were taken in field at 1.5, 2.2 and 3 m depth to observe the groundwater level effect
Mohammad Subzar Malik +2 more
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Annual soil temperature evolution
Il Nuovo Cimento C, 1991A model to study the annual behaviour of the temperature of a homogeneous solid (considered like a semispace) will be presented in this paper. The model gives the temperature of the solid at any time and at any depth. It assumes the solar flux as the incoming flux, constant atmospheric effects and a simple expression for the outgoing flux.
PUGNAGHI, Sergio, S. VINCENZI
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Soil temperature regime and vulnerability due to extreme soil temperatures in Croatia
Theoretical and Applied Climatology, 2015Soil temperature is an important factor within the climate system. Changes of trends in soil temperature and analysis of vulnerability due to heat stress can provide useful information on climate change. In this paper, the soil temperature regime was analyzed on seasonal and annual scales at depths of 2, 5, 10, 20, 30, and 50 cm at 26 sites in Croatia ...
Sviličić, Petra +3 more
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Journal of Geophysical Research: Atmospheres
Abstract The memories of soil moisture (SM) and soil temperature (ST) modulate the effect of land surface on climate prediction on monthly and longer timescales. Based on a Lagrangian‐based understanding of SM and ST memories, this study explores the characteristics of SM and ST memories using ERA5‐Land reanalysis data, observations ...
Yaoming Song +4 more
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Abstract The memories of soil moisture (SM) and soil temperature (ST) modulate the effect of land surface on climate prediction on monthly and longer timescales. Based on a Lagrangian‐based understanding of SM and ST memories, this study explores the characteristics of SM and ST memories using ERA5‐Land reanalysis data, observations ...
Yaoming Song +4 more
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Soil Temperature and Heat Transport in Soils
2018Soil temperature varies over a wide range, depending on annual and diurnal cycles of incoming solar energy and on the soil surface properties. Plants can grow when soil root zone temperatures are in the relatively narrow range 0–40 °C. Soil-water hydraulic conductivity and soil-water retention curves are functions of temperature because of the ...
Viliam Novák, Hana Hlaváčiková
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Effect of Temperature on the Consolidation of Soils
Nature, 1950IN civil engineering practice it is sometimes necessary to estimate the probable rate of settlement of structures founded on clay and other compressible soils. The settlement arises from a process in soil known as consolidation, in which the application of a load to the surface of the soil causes water to be expelled from its pores.
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Soil Temperature and Soil Heat Flux
2016The soil temperature regime depends on its thermal properties (specific heat, thermal conductivity, thermal diffusivity and thermal admittance). The main factors affecting the thermal regime are water content, soil texture and compaction. The rate of heating (or cooling) of the soil is proportional to its diffusivity which is higher in sandy soils. The
Francisco J. Villalobos +3 more
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Soil atmosphere and soil temperature
1987Plant roots, soil microorganisms and fauna are consumers of oxygen and producers of carbon dioxide. This gives rise under ordinary conditions to the well known carbon dioxide concentration gradient from about 50 000 ppm (5%) in soil pores to a little over 300 ppm in the general atmosphere.
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Journal of Agronomic Education, 1976
ABSTRACTTwo methods are described for simulating soil temperatures in the field that have been used for student experiments in a beginning soil physics laboratory. The first involves a simple numerical procedure that assumes soil thermal properties are constant.
R. J. Hanks, V. P. Rasmussen
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ABSTRACTTwo methods are described for simulating soil temperatures in the field that have been used for student experiments in a beginning soil physics laboratory. The first involves a simple numerical procedure that assumes soil thermal properties are constant.
R. J. Hanks, V. P. Rasmussen
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