Soil temperature (DP1.00041.001) : RELEASE-2021

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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Main Author: National Ecological Observatory Network NEON
Format: Dataset
Language:English
Published: National Ecological Observatory Network (NEON) 2021
Subjects:
Online Access:https://dx.doi.org/10.48443/zayg-n802
https://data.neonscience.org/data-products/DP1.00041.001/RELEASE-2021
id ftdatacite:10.48443/zayg-n802
record_format openpolar
spelling ftdatacite:10.48443/zayg-n802 2023-05-15T17:58:06+02:00 Soil temperature (DP1.00041.001) : RELEASE-2021 National Ecological Observatory Network NEON 2021 csv https://dx.doi.org/10.48443/zayg-n802 https://data.neonscience.org/data-products/DP1.00041.001/RELEASE-2021 en eng National Ecological Observatory Network (NEON) http://creativecommons.org/publicdomain/zero/1.0/ cc0 1.0 CC0 heat temperature soil temperature profile soil dataset Dataset 2021 ftdatacite https://doi.org/10.48443/zayg-n802 2021-11-05T12:55:41Z 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)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic heat
temperature
soil temperature
profile
soil
spellingShingle heat
temperature
soil temperature
profile
soil
National Ecological Observatory Network NEON
Soil temperature (DP1.00041.001) : RELEASE-2021
topic_facet heat
temperature
soil temperature
profile
soil
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-2021
title_short Soil temperature (DP1.00041.001) : RELEASE-2021
title_full Soil temperature (DP1.00041.001) : RELEASE-2021
title_fullStr Soil temperature (DP1.00041.001) : RELEASE-2021
title_full_unstemmed Soil temperature (DP1.00041.001) : RELEASE-2021
title_sort soil temperature (dp1.00041.001) : release-2021
publisher National Ecological Observatory Network (NEON)
publishDate 2021
url https://dx.doi.org/10.48443/zayg-n802
https://data.neonscience.org/data-products/DP1.00041.001/RELEASE-2021
genre permafrost
genre_facet permafrost
op_rights http://creativecommons.org/publicdomain/zero/1.0/
cc0 1.0
op_rightsnorm CC0
op_doi https://doi.org/10.48443/zayg-n802
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