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Journal articles on the topic 'Soil temperature'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

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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3

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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4

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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5

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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8

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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9

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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10

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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11

YLI-HALLA, M., and D. MOKMA. "Soil temperature regimes in Finland." Agricultural and Food Science 7, no. 4 (1998): 507–12. http://dx.doi.org/10.23986/afsci.5606.

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Soil temperature regime substantially influences soil classification in Soil Taxonomy particularly in temperate areas. To facilitate correct classification of soils of Finland, the temperature regimes in soils of the country were determined. The mean annual soil temperature, measured at 50 cm below soil surface, ranged from 6.4°C at the warmest site (Anjala) to 1.9°C at the coldest one (Utsjoki, Kevo), and the mean summer soil temperature from 13.7°C to 6.2°C at the same stations, all being in the range of the cryic temperature regime. The mean annual soil temperature was 2 to 5°C higher than

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12

Skowera, Barbara, and Jakub Wojkowski. "RELATION OF SOIL TEMPERATURE WITH AIR TEMPERATURE AT THE JURASSIC RIVER VALLEY." Inżynieria Ekologiczna 18, no. 1 (2017): 18–26. http://dx.doi.org/10.12912/23920629/65855.

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13

Wright, B. R., and P. J. Clarke. "Relationships between soil temperatures and properties of fire in feathertop spinifex (Triodia schinzii (Henrard) Lazarides) sandridge desert in central Australia." Rangeland Journal 30, no. 3 (2008): 317. http://dx.doi.org/10.1071/rj07049.

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Soil temperatures during wildfires are known to influence seed bank and plant resprouting dynamics in arid Australian grasslands. Nevertheless, relationships between soil temperatures and factors such as fuel load, fuel type, season of burn, time-of-day and soil moisture are poorly understood. This study used small-scale experimental burns to determine the effects of these five variables on soil temperature profiles (0–4 cm) during fire in spinifex sandridge country in the Haasts Bluff Aboriginal Reserve, west of Alice Springs. Fuel load and type were found to strongly influence soil temperatu

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14

Peplau, Tino, Christopher Poeplau, Edward Gregorich, and Julia Schroeder. "Deforestation for agriculture leads to soil warming and enhanced litter decomposition in subarctic soils." Biogeosciences 20, no. 5 (2023): 1063–74. http://dx.doi.org/10.5194/bg-20-1063-2023.

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Abstract. The climate-change-induced poleward shift of agriculture could lead to enforced deforestation of subarctic forest. Deforestation alters the microclimate and, thus, soil temperature, which is an important driver of decomposition. The consequences of land-use change on soil temperature and decomposition in temperature-limited ecosystems are not well understood. In this study, we buried tea bags together with soil temperature loggers at two depths (10 and 50 cm) in native subarctic forest soils and adjacent agricultural land in the Yukon Territory, Canada. A total of 37 plots was establ

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15

Ploeg, Antoon, and James Stapleton. "Glasshouse studies on the effects of time, temperature and amendment of soil with broccoli plant residues on the infestation of melon plants by Meloidogyne incognita and M. javanica." Nematology 3, no. 8 (2001): 855–61. http://dx.doi.org/10.1163/156854101753625353.

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AbstractThe effects of heating, over a range of temperatures and for increasing periods of time, and of adding finely chopped broccoli leaves to soil infested by Meloidogyne incognita and M. javanica on nematode infestation of melon, were studied in glasshouse experiments. There was a significant interaction between the effects of soil temperature, the period for which this temperature was maintained and broccoli amendment. At the lowest temperature tested (20°C), adding broccoli to the soil had very little effect on nematode infestation or galling of melon. Increasing the temperature of the b

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16

Barman, D., D. K. Kundu, Soumen Pal, et al. "Soil temperature prediction from air temperature for alluvial soils in lower Indo-Gangetic plain." International Agrophysics 31, no. 1 (2017): 9–22. http://dx.doi.org/10.1515/intag-2016-0034.

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AbstractSoil temperature is an important factor in biogeochemical processes. On-site monitoring of soil temperature is limited in spatiotemporal scale as compared to air temperature data inventories due to various management difficulties. Therefore, empirical models were developed by taking 30-year long-term (1985-2014) air and soil temperature data for prediction of soil temperatures at three depths (5, 15, 30 cm) in morning (0636 Indian standard time) and afternoon (1336 Indian standard time) for alluvial soils in lower Indo-Gangetic plain. At 5 cm depth, power and exponential regression mod

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17

Ylivainio, Kari, and Tommi Peltovuori. "Phosphorus acquisition by barley (Hordeum vulgare L.) at suboptimal soil temperature." Agricultural and Food Science 21, no. 4 (2012): 453–61. http://dx.doi.org/10.23986/afsci.6389.

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We studied the effects of soil temperature (8 ºC and 15 ºC) on barley growth, barley phosphorus (P) uptake and soil P solubility. Barley was grown in a pot experiment in two soils with different P fertilization histories for 22 years. The availability of P was estimated by using 33P-labeled fertilizer and calculating L-values. After cultivation for 22 years at ambient soil temperature without P fertilization (-P), soil L-value had decreased compared to soil that received annual P fertilization (P+). Low soil temperature further reduced the L-values, more in the -P soil than in the +P soil. Our

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18

Reshotkin, O. V. "Long-term dynamics of the atmospheric and soil climate of humid subtropics of Russia." Plant Biology and Horticulture: theory, innovation, no. 150 (September 30, 2019): 23–30. http://dx.doi.org/10.36305/2019-1-150-23-30.

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Aim. Identify patterns of temporal changes in the parameters of the atmospheric and soil climates of humid subtropics. Methods. The dynamics of air and soil temperature and precipitation are analyzed in the long-term and seasonal cycles with respect to the climatic normal, which is considered as a quantitative characteristic of the conditions of pedogenesis and climate variability over time. Results. The data on air temperature, precipitation and soil temperature yellow soils, formed in a subtropical wet-forest soil bioclimatic area are analyzed. It is shown that the average annual air tempera

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19

Ford, Trent W., and Justin T. Schoof. "Oppressive Heat Events in Illinois Related to Antecedent Wet Soils." Journal of Hydrometeorology 17, no. 10 (2016): 2713–26. http://dx.doi.org/10.1175/jhm-d-16-0075.1.

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Abstract Extreme heat events have been connected with antecedent soil moisture in many global regions, such that dry soils increase sensible heat content of the near-surface atmosphere and impede precipitation through boundary layer growth. However, negative soil moisture–temperature feedbacks (dry soils = higher temperatures) are founded on investigations of maximum temperature that neglect the potentially important latent heating component provided by soil moisture. In this study, the association of spring soil moisture and subsequent summer oppressive heat events is quantified, defined by e

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20

Polge, Nicholas D., and Michael Barrett. "Temperature effects on imazaquin soil bioavailability, uptake, and metabolism in corn (Zea mays)." Weed Science 45, no. 2 (1997): 198–204. http://dx.doi.org/10.1017/s0043174500092717.

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Growth chamber experiments were conducted to determine the effects of soil temperature on the response of corn to imazaquin soil residues. In a silt loam soil, 24/30 C (night/day) or 18/24 C soil temperatures caused greater inhibition of shoot growth than 12/18 C soil temperature. However, in a sandy loam soil, inhibition of corn shoot growth was maximal at 18/24 C, and there was no difference in shoot-growth inhibition between the lowest and highest temperatures. Higher soil temperatures caused greater root-growth inhibition in the sandy loam soil but not in silt loam soil. Soil temperature d

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21

Yang, Shu Rong, Wei Hsing Huang, and Shao Hung Chung. "Temperature Effects on Soil Suction for Compacted Clay Soils." Advanced Materials Research 723 (August 2013): 527–34. http://dx.doi.org/10.4028/www.scientific.net/amr.723.527.

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An investigation was conducted to determine the effects of temperature, compaction water content, and compaction efforts on soil suction of two expansive subgrade soils. For this purpose, two expansive soils were statically compacted at target water contents ranging from 5% to 20%. This made it possible to explore a broad spectrum of compaction conditions. Filter paper method and thermocouple psychrometer were used to measure soil suction at temperatures ranging from 10°C to 60°C. Experimental results show that compaction water content, compaction effort, and temperature have influences on soi

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22

Davenport, Joan R., and Carolyn DeMoranville. "529 Relationship of Soil Temperature, pH, and Organic Carbon Content to Nitrogen Release in Cranberry Soils." HortScience 34, no. 3 (1999): 537A—537. http://dx.doi.org/10.21273/hortsci.34.3.537a.

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Soluble nitrogen (ammonium and nitrate) is released when soil organic matter is 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 how soil N release is affected by soil temperature, intact soil cores were collected from sites that had received no fertilizer and placed in PVC columns. Four different soil types, representing the range of cranberry soils (sand, sanded organic soil, peat, and muck), were used

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23

Kuruppu, P. U., R. W. Schneider, and J. S. Russin. "Effects of Soil Temperature on Microsclerotia of Calonectria ilicicola and Soybean Root Colonization by this Fungus." Plant Disease 88, no. 6 (2004): 620–24. http://dx.doi.org/10.1094/pdis.2004.88.6.620.

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Field soil artificially infested with laboratory-produced microsclerotia of Calonectria ilicicola was incubated for 1, 2, 3, or 6 weeks at 20, 25, 30, 35, and 40°C. These temperatures approximate soil temperatures that were measured in soybean fields during the growing season in south Louisiana. Germinable microsclerotia were enumerated after incubation at different temperatures, and soybean seeds were planted in these soils. After 8 weeks, percent root colonization was determined as a measure of infectivity of microsclerotia. Results showed that soil temperature is a critical factor in surviv

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Czachor, Henryk, and Ľubomír Lichner. "Temperature influences water sorptivity of soil aggregates." Journal of Hydrology and Hydromechanics 61, no. 1 (2013): 84–87. http://dx.doi.org/10.2478/johh-2013-0011.

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Abstract The aim of this study was to determine the potential development of water sorptivity of soil aggregates by heating. Soil aggregates were sampled from arable layer of 5 Polish soils: Haplic Luvisol 1 from Czesławice, Haplic Luvisol 2 from Wierzchucinek, Haplic Cambisol from Felin, Gleyic Mollic Cambisol from Chylice, and Haplic Phaeozem from Grabiec. Three aggregates of each soil type with minimum diameter between 4 and 10 mm were heated in the oven for at least 3 hours at temperatures 20, 100, 200, 250, and 360ºC. After each temperature treatment the soil aggregates were conditioned a

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25

Gou, Qianqian, Changsheng Shen, and Guohua Wang. "Changes in Soil Moisture, Temperature, and Salt in Rainfed Haloxylon ammodendron Forests of Different Ages across a Typical Desert–Oasis Ecotone." Water 14, no. 17 (2022): 2653. http://dx.doi.org/10.3390/w14172653.

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Soil water and salt movement during the freeze–thaw period facilitate soil and water conservation and agroecological environment maintenance in the desert–oases transition zone of the Hexi Corridor; however, our understanding of soil salinization and the shifting water, heat, and salt states in soil ecosystems of Haloxylon ammodendron forests at different ages is poor. We analyzed the soil moisture, temperature, and salinity characteristics of Haloxylon ammodendron forests of different ages in the Hexi Corridor of Northwest China and determined their coupling. Our results indicated that shallo

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26

DeJonge, Kendall C., Huihui Zhang, Saleh Taghvaeian, and Thomas J. Trout. "Canopy Temperature Bias from Soil Variability Enhanced at High Temperatures." Transactions of the ASABE 63, no. 1 (2020): 95–104. http://dx.doi.org/10.13031/trans.13554.

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HighlightMaize canopy temperature (Tc) was evaluated among four replicates of seven irrigation treatments.Individual replicates showed Tc bias correlated with soil electroconductivity and increasing Tc.At high Tc values (above 35°C), Tc bias was up to 5.0°C among plots with the same irrigation schedule.ABSTRACT. Maize canopy temperature was monitored on a continuous basis for two growing seasons in a limited-irrigation maize experiment with seven separate irrigation treatments and four replicates of each treatment. Soil electroconductivity (EC) was measured and mapped to quantify the variation

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27

Akinyede, Rachael, Martin Taubert, Marion Schrumpf, Susan Trumbore, and Kirsten Küsel. "Temperature sensitivity of dark CO₂ fixation in temperate forest soils." Biogeosciences 19, no. 17 (2022): 4011–28. http://dx.doi.org/10.5194/bg-19-4011-2022.

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Abstract. Globally, soil temperature to 1 m depth is predicted to be up to 4 ∘C warmer by the end of this century, with pronounced effects expected in temperate forest regions. Increased soil temperatures will potentially increase the release of carbon dioxide (CO2) from temperate forest soils, resulting in important positive feedback on climate change. Dark CO2 fixation by microbes can recycle some of the released soil CO2, and CO2 fixation rates are reported to increase under higher temperatures. However, research on the influence of temperature on dark CO2 fixation rates, particularly in co

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Gardner, B. R., and C. A. Sanchez. "Soil Temperature Influences the Response of Lettuce to Phosphorus." HortScience 30, no. 4 (1995): 864A—864. http://dx.doi.org/10.21273/hortsci.30.4.864a.

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Lettuce is planted in the southwestern U.S. desert from September through December and harvested from November through April each year. During this period mean soil temperatures range from 7 to 30C. Lettuce produced on desert soils shows a large yield response to P. Soil solution P is replenished by desorption from the labile soil P fraction and this process is temperature sensitive. A field study was conducted over 6 years to evaluate the response of lettuce to soil solution P levels under different ambient soil temperature regimes. The soil temperatures under which lettuce was grown were var

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Yang, Shu-Rong, Rui-En Chang, Ya-Sin Yang, and Hsin-Fu Yeh. "Environmental Temperature Effect on Hydraulic Behavior and Stability of Shallow Slopes." Environments 10, no. 8 (2023): 134. http://dx.doi.org/10.3390/environments10080134.

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This study established a study framework to quantify the safety factors of unsaturated shallow slopes at different temperatures. This study is based on a non-isothermal soil water characteristic curve model quantifying the temperature-dependent hydraulic properties of soils. The hydraulic coupling analysis models HYDRUS 2D and The Slope Cube Module were used for finite element modeling. A slope stability analysis was performed based on the local factor of safety (LFS) theory. An increased temperature decreased the soil matric suction, suction stress, effective stress, and LFS, weakening the so

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Kyuma, Kazutake. "Soil Temperature Regime of Japanese Soils." Soil Science and Plant Nutrition 31, no. 3 (1985): 463–68. http://dx.doi.org/10.1080/00380768.1985.10557453.

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31

Borowik, Agata, and Jadwiga Wyszkowska. "Impact of temperature on the biological properties of soil." International Agrophysics 30, no. 1 (2016): 1–8. http://dx.doi.org/10.1515/intag-2015-0070.

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AbstractThe aim of the study was to determine the response of soil microorganisms and enzymes to the temperature of soil. The effect of the temperatures: 5, 10, 15, 20, and 25°C on the biological properties of soil was investigated under laboratory conditions. The study was performed using four different soils differing in their granulometric composition. It was found that 15°C was the optimal temperature for the development of microorganisms in soil. Typically, in the soil, the highest activity of dehydrogenases was observed at 10-15°C, catalase and acid phosphatase – at 15°C, alkaline phosph

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Zhan, Ming-jin, Lingjun Xia, Longfei Zhan, and Yuanhao Wang. "Recognition of Changes in Air and Soil Temperatures at a Station Typical of China’s Subtropical Monsoon Region (1961–2018)." Advances in Meteorology 2019 (December 1, 2019): 1–9. http://dx.doi.org/10.1155/2019/6927045.

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Trends in soil temperature are important but rarely reported indicators of climate change. Based on daily air and soil temperatures (depth: 0, 20, 80, and 320 cm) recorded at the Nanchang Weather Station (1961–2018), this study investigated the variation trend, abrupt changes, and years of anomalous annual and seasonal mean air and soil temperatures. The differences and relationships between annual air and soil temperatures were also analyzed. The results showed close correlations between air temperature and soil temperature at different depths. Annual and seasonal mean air and soil temperatur

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Burghignoli, A., A. Desideri, and S. Miliziano. "A laboratory study on the thermomechanical behaviour of clayey soils." Canadian Geotechnical Journal 37, no. 4 (2000): 764–80. http://dx.doi.org/10.1139/t00-010.

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This paper presents the findings of a laboratory investigation of the thermomechanical behaviour of clayey soils. The tests were performed on reconstituted and natural clayey soils using triaxial cells modified to control temperature. The range of temperatures that were investigated is from 20° to 60°C. The thermal behaviour of the clays and the influence of temperature on their mechanical behaviour were investigated separately. The analysis of the experimental results obtained in drained and undrained nonisothermal tests and during thermal consolidation made it possible to identify a link bet

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Pogačar, Tjaša, Lučka Kajfež Bogataj, Rok Kuk, and Zalika Črepinšek. "Effects of heat waves on soil temperatures in Slovenia." Italian Journal of Agrometeorology, no. 1 (July 19, 2022): 41–48. http://dx.doi.org/10.36253/ijam-1388.

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Soil temperature regulates the rate of plant growth and tells us much about the climatic characteristics of a particular site. Climate variability and extremes need to be studied and there is a large gap in knowledge about soil temperature during heat waves. Agricultural land is highly dependent on heat waves, which are becoming longer, more intense and more frequent, and it is important to monitor soil temperatures in situ to understand their changes during heat waves. Therefore, the aim of this work was to investigate how soil temperatures change at different depths during and after heat wav

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Campbell, Olivia, Natalie Umphlett, and Crystal Stiles. "To plant or not to plant? A soil temperature climatology for the Northern and Central Plains." Journal of Applied and Service Climatology 2022, no. 001 (2022): 1–11. http://dx.doi.org/10.46275/joasc.2022.01.001.

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Sufficient soil temperatures at the time of planting are essential for a well-established stand in both large-scale agriculture and recreational home gardening. Planting too early in the season increases the risk for frost damage and slow seedling growth while planting too late risks not reaching the required growing degree days (GDD) for plant maturity. In this study, a climatology of the date in which soils reach critical temperature thresholds for crops was developed for the Northern and Central Plains. At least 15 years of soil temperature data from 155 automated stations from six differen

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M., Cuneyt Bagdatli, and Balli Yigitcan. "Soil Temperature Changes (1970-2019) in Ulukışla District in Turkey by Trend Analysis Methods." International Journal of Plant Breeding and Crop Science (IJPBCS) 7, no. 2 (2020): 851–64. https://doi.org/10.5281/zenodo.4065111.

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<strong>Abstract</strong> This research was carried out in the context of evaluating the temperatures at different soil depths observed as monthly between 1970-2019 in Ulukışla district of Nigde province in Turkey. In the study, maximum, minimum and average soil temperatures at soil depths of 10, 50 and 100 cm were investigated. Sperman’s Rho, Mann-Kendall and Sen's slope method tests on soil temperature data were applied. According to trend analysis results; The general average of maximum soil temperatures of 10 cm depth was 22.0°C, minimum soil temperature values were 6.9 °

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Shtykov, Valeriy, Andrey Ponomarev, and Yuri Yanko. "On the dependence of soil freezing on humidity." Proceedings of Petersburg Transport University 21, no. 1 (2024): 22–31. http://dx.doi.org/10.20295/1815-588x-2024-01-22-31.

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Purpose: the temperatures at which soils begin to freeze during the onset of frost are of interest primarily to agricultural workers and construction workers. It was previously established that many factors influence soil freezing. However, not enough research has been carried out on the influence of individual factors on the freezing process. The article examines the influence of soil moisture on their supercooling and freezing temperatures. Methods: the studies were carried out in a microrefrigerator with three freezing modes. Results: it was found that with constant shaking, the supercoolin

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Zhang, Yulan, Lijun Chen, Zhijie Wu та Caixia Sun. "Kinetic parameters of soil β-glucosidase response to environmental temperature and moisture regimes". Revista Brasileira de Ciência do Solo 35, № 4 (2011): 1285–91. http://dx.doi.org/10.1590/s0100-06832011000400022.

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Soil β-glucosidase participates in the final step of cellulose biodegradation. It is significant in the soil C cycle and is used as an indicator of the biological fertility of soil. However, the response of its kinetic parameters to environmental temperature and moisture regimes is not well understood. This study tested the β-glucosidase response in the main agricultural soils (black soil, albic soil, brown soil, and cinnamon soil) of Northeast China. Incubation tests were conducted to measure the kinetic parameters Km, Vmax or Vmax/Km of soil β-glucosidase at environmental temperatures of 10,

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Zimmermann, M., K. Davies, V. T. V. Peña de Zimmermann, and M. I. Bird. "Impact of temperature and moisture on heterotrophic soil respiration along a moist tropical forest gradient in Australia." Soil Research 53, no. 3 (2015): 286. http://dx.doi.org/10.1071/sr14217.

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Tropical forests represent the largest store of terrestrial carbon (C) and are potentially vulnerable to climatic variations and human impact. However, the combined influence of temperature and precipitation on aboveground and belowground C cycling in tropical ecosystems is not well understood. To simulate the impact of climate (temperature and rainfall) on soil C heterotrophic respiration rates of moist tropical forests, we translocated soil cores among three elevations (100, 700 and 1540 m a.s.l.) representing a range in mean annual temperature of 10.9°C and in rainfall of 6840 mm. Initial s

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Adekanmbi, Adetunji Alex, Laurence Dale, Liz Shaw, and Tom Sizmur. "Differential temperature sensitivity of intracellular metabolic processes and extracellular soil enzyme activities." Biogeosciences 20, no. 11 (2023): 2207–19. http://dx.doi.org/10.5194/bg-20-2207-2023.

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Abstract. Predictions concerning the feedback of soil heterotrophic respiration to a warming climate often do not differentiate between the extracellular and intracellular steps involved in soil organic matter decomposition. This study examined the temperature sensitivities of intracellular metabolic processes and extracellular soil enzyme activities and how they are influenced by previous temperatures. We pre-incubated soils at 5, 15, or 26 ∘C to acclimatize the microbial communities to different thermal regimes for 60 d before measuring potential activities of β-glucosidase and chitinase (ex

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Nazarova, Larisa. "White Sea catchment area: changes in soil temperature." E3S Web of Conferences 462 (2023): 03053. http://dx.doi.org/10.1051/e3sconf/202346203053.

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In the situation of climate warming, no less important than changes in air temperature are estimates of changes in soil temperature both on the surface and at different depths. The article examines the current state and changes in the thermal regime of soils in the White Sea catchment area based on long-term data from weather stations located in the study area. Changes in mean annual and monthly soil temperatures were estimated for the new reference period 1991-2020. The analysis shows that the temperatures on the soil surface and at depths have increased since the beginning of the 21st centur

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Saputro, Wira Hadi, and Dan Rusdiansyah. "Study of shear strength between laterite soil due to temperature influence based on laboratory scale." Technium: Romanian Journal of Applied Sciences and Technology 27 (February 7, 2025): 41–47. https://doi.org/10.47577/technium.v27i.12504.

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South Kalimantan is a large wetland with an area of 382,272 hectares (ha). The condition of wetland with soft soil types in this area, especially peat soil can initiate fires during the dry season because the water content in the land decreases drastically. Moreover, fires that occur on peat soil land with road constructions do cause the temperature around the land to increase. The increment of this temperature can affect the physical and mechanical properties of the embankment/laterite soil. Therefore, this study aimed to determine the influence of hot temperatures on shear strength between

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Hammermeister, A. M., D. S. Chanasyk, and M. A. Naeth. "Fly ash influence on near-surface temperature of a clay loam soil." Canadian Journal of Soil Science 78, no. 2 (1998): 345–50. http://dx.doi.org/10.4141/s97-058.

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It has been suggested that fly ash, when applied as a soil amendment, would increase soil temperature. However, no quantitative data have been provided to support this hypothesis. This hypothesis was tested on four fly ash treatments (0, 100, 200, and 400 t ha−1) applied to clay loam soil in a randomized block design. Bi-hourly soil temperatures were measured on 3 summer days over 2 yr, and afternoon temperatures were measured on randomly selected spring days at 5-, 10-, and 20-cm depths in the four fly ash treatments. Temperatures were measured in conjunction with surface bulk density, water

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Oralkhan, Sultashova. "Modeling of Temperature Mode of the Soil." International Journal of Psychosocial Rehabilitation 24, no. 4 (2020): 6057–68. http://dx.doi.org/10.37200/ijpr/v24i4/pr2020416.

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Leung, Andrew C. W., William A. Gough, and Tanzina Mohsin. "Analysing Historical and Modelling Future Soil Temperature at Kuujjuaq, Quebec (Canada): Implications on Aviation Infrastructure." Forecasting 4, no. 1 (2022): 95–125. http://dx.doi.org/10.3390/forecast4010006.

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The impact of climate change on soil temperatures at Kuujjuaq, Quebec in northern Canada is assessed. First, long-term historical soil temperature records (1967–1995) are statistically analyzed to provide a climatological baseline for soils at 5 to 150 cm depths. Next, the nature of the relationship between atmospheric variables and soil temperature are determined using a statistical downscaling model (SDSM) and National Centers for Environmental Prediction (NCEP), a climatological data set. SDSM was found to replicate historic soil temperatures well and used to project soil temperatures for t

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Wilson, Brian, Subhadip Ghosh, Phoebe Barnes, and Paul Kristiansen. "Drying temperature effects on bulk density and carbon density determination in soils of northern New South Wales." Soil Research 47, no. 8 (2009): 781. http://dx.doi.org/10.1071/sr09022.

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There is a widespread and growing need for information relating to soil condition and changes in response to land management pressures. To provide the information needed to quantify land management effects on soil condition, monitoring systems are now being put in place and these programs will generate large numbers of samples. Streamlined procedures for the analysis of large sample numbers are therefore required. Bulk density (BD) is considered to be one of several key indicators for measuring soil physical condition, and is also required to estimate soil carbon density. The standard analytic

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Medellu, Christophil, Soemarno, Marsoedi, and Sigfried Berhimpon. "Temporal Variation and Respons of Mangrove Soil on Solar Illumination Changes." JOURNAL OF TROPICAL SOILS 17, no. 2 (2012): 165. http://dx.doi.org/10.5400/jts.2012.v17i2.165-172.

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Research on soil temperature in mangrove forest is a part of the mangrove ecosystem microclimate research. Studieson microclimate variables interaction, including soil temperature is important and interesting because it is associatedwith ecosystem and environmental changes, and the biota living in it. This study developed a mathematical modelingof soil temperatures and solar illumination in mangrove forest and the surrounding environment. Mathematicalmodeling function was constructed using data measured on three transects which different in ecosystem condition.The results showed that the mathe

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Paré, D., R. Boutin, G. R. Larocque, and F. Raulier. "Effect of temperature on soil organic matter decomposition in three forest biomes of eastern Canada." Canadian Journal of Soil Science 86, Special Issue (2006): 247–56. http://dx.doi.org/10.4141/s05-084.

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The sensitivity of soil organic matter decomposition to temperature change is critical tothe global carbon balance and to whether soils will respond with positive feedback to climate change. Forest cover determines litter composition, which controls to a large extent soil organic matter quality and its sensitivity to temperature. The effect of temperature on soil organic matter decomposition was studied along a latitudinal gradient encompassing sugar maple, balsam fir and black spruce forest types. Long-term laboratory soil incubations conducted at four different temperatures were used to disc

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Polyakov, D. G., A. G. Ryabukha, T. A. Arkhangelskaya, and I. V. Kovda. "Freezing of Chalk Cryomorphic Soil Complexes of the Orenburg Region: Temperature Regime and Cryogenic Processes in the Soil Profile." Počvovedenie, no. 6 (December 19, 2024): 845–60. https://doi.org/10.31857/s0032180x24060056.

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The dynamics of the temperature of conjugated soils of a paleocryogenic soil complex on chalk sediments in the Orenburg region is studied. Temperature measurements were combined with the investigation of cryogenic features. The freezing point of soil moisture was determined in the laboratory. A significant heterogeneity of the temperature field within the soil complex was revealed. During the autumn–winter, the soil of micro-elevation was colder than the soils of micro-depression and micro-slope, and in the spring-summer period, the micro-slope warmed up faster than the micro-elevation and mic

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Vasilescu, Roxana, Kexin Yin, Anne-Laure Fauchille, et al. "Influence of thermal cycles on the deformation of soil-pile interface in energy piles." E3S Web of Conferences 92 (2019): 13004. http://dx.doi.org/10.1051/e3sconf/20199213004.

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Energy piles are double purpose foundation elements used both for transferring loads to the soil and temperature regulation in buildings. The response of the pile-soil interface is influenced by daily and seasonal temperature variations. In order to assess the impact of thermal cycles on the mobilization of shear strength in energy piles, a series of saturated soil-concrete interface direct shear tests were performed in the laboratory for different temperature gradients with a new interface direct shear device adapted for thermomechanical loading. As natural soils are very complex due to a hig

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