Soil temperature (DP1.00041.001) : RELEASE-2022
Soil temperature is measured at various depths below the soil surface from approximately 2 cm up to 200 cm at non-permafrost sites (up to 300 cm at Alaskan sites). Soil temperature influences the rate of biogeochemical cycling, decomposition, and root and soil biota activity. In addition, soil tempe...
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National Ecological Observatory Network (NEON)
2022
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Online Access: | https://dx.doi.org/10.48443/9e56-pj39 https://data.neonscience.org/data-products/DP1.00041.001/RELEASE-2022 |
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ftdatacite:10.48443/9e56-pj39 2023-05-15T17:58:07+02:00 Soil temperature (DP1.00041.001) : RELEASE-2022 National Ecological Observatory Network NEON 2022 csv https://dx.doi.org/10.48443/9e56-pj39 https://data.neonscience.org/data-products/DP1.00041.001/RELEASE-2022 en eng National Ecological Observatory Network (NEON) heat profile soil soil temperature temperature Dataset dataset 2022 ftdatacite https://doi.org/10.48443/9e56-pj39 2022-02-09T13:00:22Z Soil temperature is measured at various depths below the soil surface from approximately 2 cm up to 200 cm at non-permafrost sites (up to 300 cm at Alaskan sites). Soil temperature influences the rate of biogeochemical cycling, decomposition, and root and soil biota activity. In addition, soil temperature can impact the hydrologic cycle since it controls whether soil water is in a liquid or solid state. Measurements are made in vertical profiles consisting of up to nine depths in all five instrumented soil plots at each terrestrial site, and presented as 1-minute and 30-minute averages. Latency: Data collected in any given month are published during the second full week of the following month. : When possible the soil plots were arranged in a transect with the first plot approximately 15-40 m from the tower in the expected dominant airshed. The middle of airshed was used as the transect vector and plot spacing was based on the distance required for surface soil temperature and moisture measurements to be spatially independent at the 1 hectare scale during site characterization (capped at approximately 40 m due to logistical constraints). Soil plots were microsited as necessary to avoid obstacles (e.g., boulders, streams, and paths) and more compact plot layouts were used at small sites. Soil temperature is measured at up to nine depths within each plot, with the mid-point of the shallowest sensors at approximately 2, 6, 16, and 26 cm. Depths for deeper sensors vary among sites and are based on megapit soil horizon data (NEON.DP1.00097) and depth to restrictive feature (see NEON.DOC.003146). Instrumentation: Thermometrics - Climate RTD 100-ohm Probe Dataset permafrost DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
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English |
topic |
heat profile soil soil temperature temperature |
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heat profile soil soil temperature temperature National Ecological Observatory Network NEON Soil temperature (DP1.00041.001) : RELEASE-2022 |
topic_facet |
heat profile soil soil temperature temperature |
description |
Soil temperature is measured at various depths below the soil surface from approximately 2 cm up to 200 cm at non-permafrost sites (up to 300 cm at Alaskan sites). Soil temperature influences the rate of biogeochemical cycling, decomposition, and root and soil biota activity. In addition, soil temperature can impact the hydrologic cycle since it controls whether soil water is in a liquid or solid state. Measurements are made in vertical profiles consisting of up to nine depths in all five instrumented soil plots at each terrestrial site, and presented as 1-minute and 30-minute averages. Latency: Data collected in any given month are published during the second full week of the following month. : When possible the soil plots were arranged in a transect with the first plot approximately 15-40 m from the tower in the expected dominant airshed. The middle of airshed was used as the transect vector and plot spacing was based on the distance required for surface soil temperature and moisture measurements to be spatially independent at the 1 hectare scale during site characterization (capped at approximately 40 m due to logistical constraints). Soil plots were microsited as necessary to avoid obstacles (e.g., boulders, streams, and paths) and more compact plot layouts were used at small sites. Soil temperature is measured at up to nine depths within each plot, with the mid-point of the shallowest sensors at approximately 2, 6, 16, and 26 cm. Depths for deeper sensors vary among sites and are based on megapit soil horizon data (NEON.DP1.00097) and depth to restrictive feature (see NEON.DOC.003146). Instrumentation: Thermometrics - Climate RTD 100-ohm Probe |
format |
Dataset |
author |
National Ecological Observatory Network NEON |
author_facet |
National Ecological Observatory Network NEON |
author_sort |
National Ecological Observatory Network NEON |
title |
Soil temperature (DP1.00041.001) : RELEASE-2022 |
title_short |
Soil temperature (DP1.00041.001) : RELEASE-2022 |
title_full |
Soil temperature (DP1.00041.001) : RELEASE-2022 |
title_fullStr |
Soil temperature (DP1.00041.001) : RELEASE-2022 |
title_full_unstemmed |
Soil temperature (DP1.00041.001) : RELEASE-2022 |
title_sort |
soil temperature (dp1.00041.001) : release-2022 |
publisher |
National Ecological Observatory Network (NEON) |
publishDate |
2022 |
url |
https://dx.doi.org/10.48443/9e56-pj39 https://data.neonscience.org/data-products/DP1.00041.001/RELEASE-2022 |
genre |
permafrost |
genre_facet |
permafrost |
op_doi |
https://doi.org/10.48443/9e56-pj39 |
_version_ |
1766166659563782144 |