Relevant bibliographies by topics / Soil temperature

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Soil temperature'

Author: Grafiati
Published: 4 June 2021
Last updated: 25 July 2025

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Journal articles on the topic "Soil temperature"

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HAYHOE, H. N., C. TARNOCAI, and L. M. DWYER. "SOIL MANAGEMENT AND VEGETATION EFFECTS ON MEASURED AND ESTIMATED SOIL THERMAL REGIMES IN CANADA." Canadian Journal of Soil Science 70, no. 1 (1990): 61–71. http://dx.doi.org/10.4141/cjss90-007.

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Observations at sites in British Columbia, the Yukon, Manitoba and Nova Scotia over a range of soils, managements and vegetation were used to assess variation in soil temperature. The annual soil temperature regime was compared with estimates derived from a macroclimate model which was developed for mineral soils that are level, well to moderately well drained, and covered by short grass. In general, this study showed the dampening effect of vegetation cover on soil temperature and suggested the further dampening effect of an organic layer on the soil surface. However, soil temperatures for cu
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Lugo-Camacho, Jorge L., Samuel J. Indorante, John M. Kabrick, and Miguel A. Muñoz. "Soil temperature variations between a Typic Fragiudults and a Typic Paleudults in the Ozark Highlands of Missouri." Journal of Agriculture of the University of Puerto Rico 105, no. 2 (2022): 125–41. http://dx.doi.org/10.46429/jaupr.v105i2.20071.

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Soil temperature measurements from a Soil Climate Analysis Network (SCAN) monitoring site in the Ozark Highlands Major Land Resource Area (MLRA 116A) were evaluated on landscapes comprising Typic Fragiudults (Scholten series) and Typic Paleudults (Poynor series). The five soil forming factors were similarfor both soils, with the major difference between the adjacent soils being a fragipan in the Scholten series. Air and soil temperatures were collected from a weather station of the USDA-Natural Resources Conservation Service near the border of the mesic soil temperature regime and udic soil mo
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Davenport, Joan R., and Carolyn DeMoranville. "Temperature Influences Nitrogen Release Rates in Cranberry Soils." HortScience 39, no. 1 (2004): 80–83. http://dx.doi.org/10.21273/hortsci.39.1.80.

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Native nitrogen is released when soils are mineralized. The amount of N released by this process depends on the amount of organic matter present and soil temperature. Cranberry (Vaccinium macrocarpon Ait.) grows in acidic soils with a wide range in organic matter content. To evaluate release of cranberry soil N at varied soil temperatures, intact soils were collected from sites that had received no fertilizer. Soils were cored and placed in polyvinyl chloride (PVC) columns 20 cm deep × 5 cm in diameter. Four different soil types, representing the array of conditions in cranberry soil (mineral,
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Nichols, Dale S. "Temperature of upland and peatland soils in a north central Minnesota forest." Canadian Journal of Soil Science 78, no. 3 (1998): 493–509. http://dx.doi.org/10.4141/s96-030.

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Soil temperature strongly influences physical, chemical, and biological activities in soil. However, soil temperature data for forest landscapes are scarce. For 6 yr, weekly soil temperatures were measured at two upland and four peatland sites in north central Minnesota. One upland site supported mature aspen forest, the other supported short grass. One peatland site was forested with black spruce, one supported tall willow and alder brush, and two had open vegetation — sedges and low shrubs. Mean annual air temperature averaged 3.6 °C. Mean annual soil temperatures at 10- to 200-cm depths ran
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Liu, J., C. Geng, Y. Mu, Y. Zhang, and H. Wu. "Exchange of carbonyl sulfide (COS) between the atmosphere and various soils in China." Biogeosciences Discussions 6, no. 6 (2009): 10557–82. http://dx.doi.org/10.5194/bgd-6-10557-2009.

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Abstract. Using a dynamic enclosure, the exchange fluxes of carbonyl sulfide (COS) between the atmosphere and 18 soils from 10 provinces in China were investigated. The emission or uptake of COS from the soils was highly dependent on the soil type, soil temperature, soil moisture, and atmospheric COS mixing ratio. In general, with the only exception being paddy soils, the soils in this investigation acted as sinks for atmospheric COS under wide ranges of soil temperature and soil moisture. Two intensively investigated wheat soils and one forest soil, had optimal soil temperatures for COS uptak
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Liu, J., C. Geng, Y. Mu, Y. Zhang, Z. Xu, and H. Wu. "Exchange of carbonyl sulfide (COS) between the atmosphere and various soils in China." Biogeosciences 7, no. 2 (2010): 753–62. http://dx.doi.org/10.5194/bg-7-753-2010.

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Abstract. Using a dynamic enclosure, the exchange rates of carbonyl sulfide (COS) between the atmosphere and 18 soils from 12 provinces in China were investigated. The emission or uptake of COS from the soils was highly dependent on the soil type, soil temperature, soil moisture, and atmospheric COS mixing ratio. In general, with the only exception being paddy soils, the soils in this investigation acted as sinks for atmospheric COS under wide ranges of soil temperature and soil moisture. Two intensively investigated wheat soils and one forest soil had optimal soil temperatures for COS uptake
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Guicharnaud, R., O. Arnalds, and G. I. Paton. "Short term changes of microbial processes in Icelandic soils to increasing temperatures." Biogeosciences 7, no. 2 (2010): 671–82. http://dx.doi.org/10.5194/bg-7-671-2010.

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Abstract. Temperature change is acknowledged to have a significant effect on soil biological processes and the corresponding sequestration of carbon and cycling of nutrients. Soils at high latitudes are likely to be particularly impacted by increases in temperature. Icelandic soils experience unusually frequent freeze and thaw cycles compare to other Arctic regions, which are increasing due to a warming climate. As a consequence these soils are frequently affected by short term temperature fluctuations. In this study, the short term response of a range of soil microbial parameters (respiration
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Akter, M., MA Miah, MM Hassan, MN Mobin, and MA Baten. "Textural Influence on Surface and Subsurface Soil Temperatures under Various Conditions." Journal of Environmental Science and Natural Resources 8, no. 2 (2016): 147–51. http://dx.doi.org/10.3329/jesnr.v8i2.26882.

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An experiment was conducted at the field laboratory of Department of Environmental Science, Bangladesh Agricultural University, Mymensingh to study the textural influence on surface and subsurface soil temperatures under various conditions. The experiment consisted of four types of soil (red, sandy, clay and peat). Observations were made at three conditions viz. bare, moist and vegetation cover. Sandy soil at bare condition showed the highest surface temperature followed by peat, red and clay soils. Sand surface produced nearly 10ºC higher values than from clay soil at around midday hours. In
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Polyakov, Dmitry G., Anna G. Ryabukha, Tatiana Al Arkhangelskaya, and Irina V. Kovda. "Winter temperature regime of thufur soils on gazha sediments in Orenburg oblast." Lomonosov Soil Science Journal 79, no. 4, 2024 (2024): 114–21. https://doi.org/10.55959/msu0137-0944-17-2024-79-4-114-121.

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Winter temperature regime was studied for soils of thufur field formed on gazha sediments within the first terrace above the floodplain, and for the dark humus soil formed under the conditions which were closer to zonal ones. The temperature of atmospheric air, that of soil surface under snow and soil temperatures at the depths of 5–120 cm were measured with autonomous temperature recorders. The surface temperature of soil under snow depended on the snow depth. In the thufur center the sum of surface temperatures for the period from December 10 to March 30 was equal to –387°C, and in the micro
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Rankinen, K., T. Karvonen, and D. Butterfield. "A simple model for predicting soil temperature in snow-covered and seasonally frozen soil: model description and testing." Hydrology and Earth System Sciences 8, no. 4 (2004): 706–16. http://dx.doi.org/10.5194/hess-8-706-2004.

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Abstract. Microbial processes in soil are moisture, nutrient and temperature dependent and, consequently, accurate calculation of soil temperature is important for modelling nitrogen processes. Microbial activity in soil occurs even at sub-zero temperatures so that, in northern latitudes, a method to calculate soil temperature under snow cover and in frozen soils is required. This paper describes a new and simple model to calculate daily values for soil temperature at various depths in both frozen and unfrozen soils. The model requires four parameters: average soil thermal conductivity, specif
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Dissertations / Theses on the topic "Soil temperature"

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Alvenäs, Gunnel. "Evaporation, soil moisture and soil temperature of bare and cropped soils /." Uppsala : Swedish Univ. of Agricultural Sciences (Sveriges lantbruksuniv.), 1999. http://epsilon.slu.se/avh/1999/91-576-5714-9.pdf.

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Franks, Carol Dawn. "Temperature, moisture and albedo properties of Arizona soils." Thesis, The University of Arizona, 1985. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1985_263_sip1_w.pdf&type=application/pdf.

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Chang, Chao-Ting. "Soil water availability regulates soil respiration temperature dependence in Mediterranean forests." Doctoral thesis, Universitat de Barcelona, 2017. http://hdl.handle.net/10803/406082.

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The variations of ecosystem and soil respiration are mainly driven by temperature and precipitation, but the importance of temperature and precipitation could vary across temporal and spatial. At diurnal to annual temporal scales, ecosystem and soil respiration generally increase with average annual temperature, but very low or very high soil moisture has been shown to diminish the temperature response of respiration. Therefore, in water-limited ecosystem, such as the Mediterranean region where the seasonal pattern is characterized with significant summer drought, precipitation patterns are li
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Burns, Nancy Rosalind. "Soil organic matter stability and the temperature sensitivity of soil respiration." Thesis, University of Edinburgh, 2012. http://hdl.handle.net/1842/9922.

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Soil respiration is an important source of atmospheric CO2, with the potential for large positive feedbacks with global warming. The size of these feedbacks will depend on the relative sensitivity to temperature of very large global pools of highly stable soil organic matter (SOM), with residence times of centuries or longer. Conflicting evidence exists as to the relationships between temperature sensitivity of respiration and stability of SOM, as well as the temperature sensitivity of individual stabilisation mechanisms. This PhD considers the relationship between different stabilisation mech
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Hartley, Iain P. "The response of soil respiration to temperature." Thesis, University of York, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.434021.

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Attalla, Daniela, and Wu Jennifer Tannfelt. "Automated Greenhouse : Temperature and soil moisture control." Thesis, KTH, Maskinkonstruktion (Inst.), 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-184599.

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In this thesis an automated greenhouse was built with the purpose of investigating the watering system’s reliability and if a desired range of temperatures can be maintained. The microcontroller used to create the automated greenhouse was an Arduino UNO. This project utilizes two different sensors, a soil moisture sensor and a temperature sensor. The sensors are controlling the two actuators which are a heating fan and a pump. The heating fan is used to change the temperature and the pump is used to water the plant. The watering system and the temperature control system was tested both separat
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Al-Ali, Abdullah Mubarak Abdulmohsen. "Temperature effects on fine-grained soil erodibility." Thesis, Kansas State University, 2016. http://hdl.handle.net/2097/32514.

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Master of Science<br>Civil Engineering<br>Stacey Tucker<br>Recent climate changes may affect the stability of our infrastructure in many ways. This study investigated the effects of fine-grained soil temperature on erosion rate. If climate change is shown to affect the erodibility of soils the impacts must be identified to monitor the stability of existing infrastructure, improve design of levees and structures founded in erosive environments, and to prevent sediment loss and stream meanders. Fine-grained soil erosion is complicated by the dynamic linkage of multiple parameters, including phys
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Mampana, Reedah Makgwadi. "Cropping system effects on soil water, soil temperature and dryland maize productivity." Diss., University of Pretoria, 2014. http://hdl.handle.net/2263/43165.

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Improved soil water conservation has become an important subject in semi-arid areas due to low and erratic rainfall which is often combined with higher temperatures to provide unsuitable conditions for successful crop productivity. Dryland agriculture remains vulnerable to yield losses in these areas. This calls for implementation of conservation agricultural practices that would improve dryland maize productivity. An on-station field trial was started in 2007 at Zeekoegat experimental farm (24 kilometers north of Pretoria), to establish the effect of different conservation agriculture practic
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Chen, Ying 1957. "Soil thermal regime resulting from reduced tillage systems." Thesis, McGill University, 1992. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=41106.

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The soil thermal regime is important to the soil and plant environment, being an influential factor in determining many processes in soil.<br>Changes in soil bulk density, soil surface reflectance and soil temperature changes with depth and time were studied theoretically and experimental as a function of variable soil properties, soil surface state, crop cover and atmospheric conditions.<br>A field experiment was carried out on sandy and clayey soils with each plot being subjected to a consistent tillage and fertilizer history of either conventional ploughing, reduced energy disking or zero t
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Adu-Gyamfi, Kwame. "Laboratory calibration of soil moisture, resistivity, and temperature probe - Capacitance probe." Ohio : Ohio University, 2001. http://www.ohiolink.edu/etd/view.cgi?ohiou1173385776.

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Books on the topic "Soil temperature"

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Stathers, Robert John. Forest soil temperature manual. Canada/BC Economic & Regional Development Agreement, 1990.

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Stathers, Robert John. Forest soil temperature manual. Ministry of Forests, Research Branch, 1990.

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Curtis, C. S. Soil temperature bibliography with abstracts. High Plains Climate Center, Dept. of Agricultural Meteorology, University of Nebraska, 1995.

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Hanks, R. J. Applied soil physics: Soil water and temperature applications. 2nd ed. Springer-Verlag, 1992.

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Hussein, J. Soil temperatures in Zimbabwe. Dept. [of] Land Management, Faculty of Agriculture, University of Zimbabwe, 1986.

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Hughes, Paul A. Water tables, soil temperatures, and morphological characteristics in selected Maine soils. Dept. of Plant, Soil, and Environmental Sciences, University of Maine, 1993.

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Franco, E. P. Cardoso. Os regimes, térmico e de humidade, nos solos da república popular de Angola. Ministério do Planeamento e da Administração do Território, Secretaria de Estado da Ciência e Tecnologia, Instituto de Investigação Científica Tropical, 1993.

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Franco, E. P. Cardoso. Contribuição para o estudo do pedoclima no arquipélago da Madeira. Secretaria Regional da Economia, Instituto de Investigação Científica Tropical, 1990.

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Vose, James M. A soil temperature model for closed canopied forest stands. Southeastern Forest Experiment Station, 1991.

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Vose, James M. A soil temperature model for closed canopied forest stands. U.S. Dept. of Agriculture, Forest Service, Southeastern Forest Experiment Station, 1991.

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Book chapters on the topic "Soil temperature"

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Novak, Michael D. "Soil Temperature." In Agronomy Monographs. American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America, 2015. http://dx.doi.org/10.2134/agronmonogr47.c6.

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Jeffrey, David W. "Soil atmosphere and soil temperature." In Soil~Plant Relationships. Springer Netherlands, 1987. http://dx.doi.org/10.1007/978-94-011-6076-6_9.

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Ochsner, Tyson E. "Measuring Soil Temperature." In Soil Science Step-by-Step Field Analysis. American Society of Agronomy and Soil Science Society of America, 2015. http://dx.doi.org/10.2136/2008.soilsciencestepbystep.c18.

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Villalobos, Francisco J., Luca Testi, Luciano Mateos, and Elias Fereres. "Soil Temperature and Soil Heat Flux." In Principles of Agronomy for Sustainable Agriculture. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-46116-8_6.

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Villalobos, Francisco J., Luca Testi, Luciano Mateos, and Elias Fereres. "Soil Temperature and Soil Heat Flux." In Principles of Agronomy for Sustainable Agriculture. Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-69150-8_6.

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Novák, Viliam, and Hana Hlaváčiková. "Soil Temperature and Heat Transport in Soils." In Applied Soil Hydrology. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-030-01806-1_20.

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Buchan, Graeme D. "Temperature Effects in Soil." In Encyclopedia of Agrophysics. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-3585-1_170.

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Raney, F. C., and Yoshiaki Mihara. "Water and Soil Temperature." In Irrigation of Agricultural Lands. American Society of Agronomy, 2015. http://dx.doi.org/10.2134/agronmonogr11.c58.

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Mukherjee, Swapna. "Soil Air and Temperature." In Current Topics in Soil Science. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-92669-4_10.

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Hanks, R. J. "Soil Heat Flow and Temperature." In Applied Soil Physics. Springer New York, 1992. http://dx.doi.org/10.1007/978-1-4612-2938-4_5.

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Conference papers on the topic "Soil temperature"

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Dattatreya, Sneha, Manoj Sain, Archit Khurana, K. Jena, and Gaurav Chatterjee. "Enhanced Soil Nutrient-NPK Measurement Using Electrical Conductivity and Temperature." In 2024 International Conference on Communication, Control, and Intelligent Systems (CCIS). IEEE, 2024. https://doi.org/10.1109/ccis63231.2024.10931890.

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Nakayama, C., H. Arima, T. Katsumata, H. Aizawa, and S. Komuro. "Temperature response measurement of soil." In 2007 International Conference on Control, Automation and Systems. IEEE, 2007. http://dx.doi.org/10.1109/iccas.2007.4406721.

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Ma, Hongzhang, and Qinhuo Liu. "The Analysis of the Difference between Infrared Soil Temperature and L Band Effective Soil Temperature." In 2011 International Workshop on Multi-Platform/Multi-Sensor Remote Sensing and Mapping (M2RSM). IEEE, 2011. http://dx.doi.org/10.1109/m2rsm.2011.5697425.

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Vitkova, Justina. "SOIL TEMPERATURE REGIME IN TOP SOIL LAYER WITH BIOCHAR AMENDMENT." In 17th International Multidisciplinary Scientific GeoConference SGEM2017. Stef92 Technology, 2017. http://dx.doi.org/10.5593/sgem2017/32/s13.068.

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Tian, Hongwei, Linmao Ye, and Haibo Chen. "Study on effect of soil temperature on FDR soil moisture sensor in frozen soil." In Third International Conference on Photonics and Image in Agriculture Engineering (PIAGENG 2013), edited by Honghua Tan. SPIE, 2013. http://dx.doi.org/10.1117/12.2019726.

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Claverie, Etienne, Jeremie Lecoeur, Veronique Letort, and Paul-Henry Cournede. "Modeling soil temperature to predict emergence." In 2016 IEEE International Conference on Functional-Structural Plant Growth Modeling, Simulation, Visualization and Applications (FSPMA). IEEE, 2016. http://dx.doi.org/10.1109/fspma.2016.7818285.

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Popiel, C. O., Janusz Wojtkowiak, and B. Biernacka. "MEASUREMENTS OF TEMPERATURE DISTRIBUTIONS IN SOIL." In Thermal Sciences 2000. Proceedings of the International Thermal Science Seminar Bled. Begellhouse, 2000. http://dx.doi.org/10.1615/ichmt.2000.thersieprocvol2.40.

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Popiel, C. O., and B. Biernacka. "MEASUREMENTS OF TEMPERATURE DISTRIBUTIONS IN SOIL." In Thermal Sciences 2000. Proceedings of the International Thermal Science Seminar Bled. Begellhouse, 2000. http://dx.doi.org/10.1615/ichmt.2000.thersieprocvol2thersieprocvol1.210.

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Holmes, T., and T. Jackson. "Soil temperature error propagation in passive microwave retrieval of soil moisture." In 2010 11th Specialist Meeting on Microwave Radiometry and Remote Sensing of the Environment (MicroRad 2010). IEEE, 2010. http://dx.doi.org/10.1109/microrad.2010.5559589.

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"Reviving the old soil solarization method by monitoring the soil temperature." In Protected Cultivation of High-Value Crops under Changing Climate Conditions. Food and Fertilizer Technology Center for the Asian and Pacific Region, 2017. http://dx.doi.org/10.56669/sskc1609.

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Reports on the topic "Soil temperature"

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Frankenstein, Susan. FASST Soil Moisture, Soil Temperature: Original Versus New. Defense Technical Information Center, 2008. http://dx.doi.org/10.21236/ada483823.

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Vas, Dragos, Elizabeth Corriveau, Lindsay Gaimaro, and Robyn Barbato. Challenges and limitations of using autonomous instrumentation for measuring in situ soil respiration in a subarctic boreal forest in Alaska, USA. Engineer Research and Development Center (U.S.), 2023. http://dx.doi.org/10.21079/11681/48018.

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Subarctic and Arctic environments are sensitive to warming temperatures due to climate change. As soils warm, soil microorganisms break down carbon and release greenhouse gases such as methane (CH₄) and carbon dioxide (CO₂). Recent studies examining CO₂ efflux note heterogeneity of microbial activity across the landscape. To better understand carbon dynamics, our team developed a predictive model, Dynamic Representation of Terrestrial Soil Predictions of Organisms’ Response to the Environment (DRTSPORE), to estimate CO₂ efflux based on soil temperature and moisture estimates. The goal of this
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Montz, A., V. R. Kotamarthi, and H. Bellout. Soil carbon response to rising temperature. Office of Scientific and Technical Information (OSTI), 2012. http://dx.doi.org/10.2172/1051236.

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Gonzalez, Logan, Christopher Baker, Stacey Doherty, and Robyn Barbato. Ecological modeling of microbial community composition under variable temperatures. Engineer Research and Development Center (U.S.), 2024. http://dx.doi.org/10.21079/11681/48184.

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Soil microorganisms interact with one another within soil pores and respond to external conditions such as temperature. Data on microbial community composition and potential function are commonly generated in studies of soils. However, these data do not provide direct insight into the drivers of community composition and can be difficult to interpret outside the context of ecological theory. In this study, we explore the effect of abiotic environmental variation on microbial species diversity. Using a modified version of the Lotka-Volterra Competition Model with temperature-dependent growth ra
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Lui, Rui, Cheng Zhu, John Schmalzel, et al. Experimental and numerical analyses of soil electrical resistivity under subfreezing conditions. Engineer Research and Development Center (U.S.), 2024. http://dx.doi.org/10.21079/11681/48430.

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The engineering behavior of frozen soils is critical to the serviceability of civil infrastructure in cold regions. Among various geophysical techniques, electrical resistivity imaging is a promising technique that is cost effective and provides spatially continuous subsurface information. In this study, under freeze–thaw conditions, we carry out lab–scale 1D electrical resistivity measurements on frost–susceptible soils with varying water content and bulk density properties. We use a portable electrical resistivity meter for temporal electrical resistivity measurements and thermocouples for t
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Cook, David, and Adam Theisen. SWATS: Diurnal Trends in the Soil Temperature Report. Office of Scientific and Technical Information (OSTI), 2017. http://dx.doi.org/10.2172/1366762.

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Cook, David R. Soil Water and Temperature System (SWATS) Instrument Handbook. Office of Scientific and Technical Information (OSTI), 2016. http://dx.doi.org/10.2172/1251383.

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Cook, David R. Soil Temperature and Moisture Profile (STAMP) System Handbook. Office of Scientific and Technical Information (OSTI), 2016. http://dx.doi.org/10.2172/1332724.

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VanderGheynst, Jean, Michael Raviv, Jim Stapleton, and Dror Minz. Effect of Combined Solarization and in Solum Compost Decomposition on Soil Health. United States Department of Agriculture, 2013. http://dx.doi.org/10.32747/2013.7594388.bard.

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In soil solarization, moist soil is covered with a transparent plastic film, resulting in passive solar heating which inactivates soil-borne pathogen/weed propagules. Although solarization is an effective alternative to soil fumigation and chemical pesticide application, it is not widely used due to its long duration, which coincides with the growing season of some crops, thereby causing a loss of income. The basis of this project was that solarization of amended soil would be utilized more widely if growers could adopt the practice without losing production. In this research we examined three
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Vose, James M., and Wayne T. Swank. A Soil Temperature Model for Closed Canopied Forest Stands. U.S. Department of Agriculture, Forest Service, Southeastern Forest Experiment Station, 1991. http://dx.doi.org/10.2737/se-rp-281.

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