soil thermometer reotemp (REOTEMP Instrument Corporation)
90
Structured Review
REOTEMP Instrument Corporation
soil thermometer reotemp
Soil Thermometer Reotemp, supplied by REOTEMP Instrument Corporation, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/reotemp+soil+thermometer/reotemp+soil+thermometer/10__3390_slash_atmos10110708-79-16-19
Average 90 stars, based on 1 article reviews
Soil Thermometer Reotemp, supplied by REOTEMP Instrument Corporation, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/reotemp+soil+thermometer/reotemp+soil+thermometer/10__3390_slash_atmos10110708-79-16-19
Average 90 stars, based on 1 article reviews
soil thermometer reotemp - by Bioz Stars,
2026-09
90/100 stars
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other:Article Title: Factors influencing broadcast-herbicide control of huisache (Vachellia farnesiana) Article Snippet: Soil temperature at a depth of 30 cm at the time of Sampling:Article Title: Vegetation and elevation influence the timing and magnitude of soil CO<sub>2</sub> efflux in a humid, topographically complex watershed Article Snippet: Soil samples were taken in conjunction with HydroSense measurements in 2012 (depth: 12 cm; volume: 56.414 cm3; n= 37), and actual VWC (volumetric water content, m−3)m3)) (2lab) was calculated using Eq. (3) from Rose (2004), where w is the gravimetric water content of the soil sample (g−3 g3), ρb is the soil bulk density (g cm −3), and ρ (g cm−3) is the density of water: θlab = wρb ρ . (3) In order to calibrate field measurements of VWC (2field),√ Ka values were then regressed against 2lab to create an Eq. (4), relating √ Ka to 2 (R 2 = 0.74) such that field measurements of VWC (2field) could be converted to 2 in order to account for discrepancies in organic matter, soil bulk density, and clay content: θ = 7.0341 · (√ Ka ) + 0.0806. (4) 2 was then converted to water-filled pore space (WFPS; m−3 m3) using the soil porosity (8; m−3 m3): WFPS= θ ·8. (5) WFPS provides a more mechanistic variable that takes into account the bulk density and porosity of the soil, which influence the transport and storage capacity of the soil with regard to soil CO2. .. During each field sampling session, soil temperature (TSOIL; ◦C) was measured at 12 cm using a 12 cm |