Soil C stock and CO2 production data for Soong et al. 2021: Effects of five years of soil warming at Blodgett Forest, CA.
Abstract
Subsoils below 20 cm are an important reservoir in the global carbon cycle, but little is known about their vulnerability under climate change. We measured subsoil carbon in warmed vs control plots of a conifer forest after 4.5 years of whole-soil warming (4°C). We also measured soil CO2 efflux at the surface and soil CO2 concentrations along the soil profile. Over the 4.5 years we observed that warming resulted in a loss of subsoil carbon stocks (−33 ± 11%), primarily from unprotected particulate organic matter. Warming also stimulated a sustained 30 ± 4% increase in soil CO2 efflux due to increased CO2 production through the whole-soil profile. The observed in situ decline in subsoil carbon stocks with warming is now definitive evidence of a positive soil carbon-climate feedback, which could not be concluded based on increases in CO2 effluxes alone. This dataset comprises (1) 13C and C recovery in 2014, 2016, and 2018 1m soil cores sampled in 10cm increments. (2) Monthly surface CO2 fluxes from 2014 to 2018. (3) Monthly gas well sample [CO2] and production data. And (4) density fraction data for three depths of cores recovered in 2017.
- Authors:
-
- Corteva Agriscience; Lawrence Berkeley National Laboratory
- Dartmouth College
- Lawrence Berkeley National Laboratory
- University of Zurich
- Publication Date:
- Research Org.:
- Environmental System Science Data Infrastructure for a Virtual Ecosystem; Belowground Biogeochemistry Scientific Focus Area
- Sponsoring Org.:
- U.S. DOE > Office of Science > Biological and Environmental Research (BER)
- Subject:
- 54 ENVIRONMENTAL SCIENCES; EARTH SCIENCE > LAND SURFACE > SOILS; EARTH SCIENCE > LAND SURFACE > SOILS > CARBON; EARTH SCIENCE > LAND SURFACE > SOILS > NITROGEN; EARTH SCIENCE > LAND SURFACE > SOILS > ORGANIC MATTER; EARTH SCIENCE > LAND SURFACE > SOILS > SOIL BULK DENSITY; EARTH SCIENCE > LAND SURFACE > SOILS > SOIL GAS/AIR; EARTH SCIENCE > LAND SURFACE > SOILS > SOIL MOISTURE/WATER CONTENT; EARTH SCIENCE > LAND SURFACE > SOILS > SOIL RESPIRATION; EARTH SCIENCE > LAND SURFACE > SOILS > SOIL TEMPERATURE
- OSTI Identifier:
- 1896308
- DOI:
- https://doi.org/10.15485/1896308
Citation Formats
Soong, Jennifer, Hicks Pries, Caitlin, Castanha, Cristina, Porras, Rachel, Ofiti, Nicholas, Torn, Margaret, Schmidt, Michael, and Riley, William. Soil C stock and CO2 production data for Soong et al. 2021: Effects of five years of soil warming at Blodgett Forest, CA.. United States: N. p., 2022.
Web. doi:10.15485/1896308.
Soong, Jennifer, Hicks Pries, Caitlin, Castanha, Cristina, Porras, Rachel, Ofiti, Nicholas, Torn, Margaret, Schmidt, Michael, & Riley, William. Soil C stock and CO2 production data for Soong et al. 2021: Effects of five years of soil warming at Blodgett Forest, CA.. United States. doi:https://doi.org/10.15485/1896308
Soong, Jennifer, Hicks Pries, Caitlin, Castanha, Cristina, Porras, Rachel, Ofiti, Nicholas, Torn, Margaret, Schmidt, Michael, and Riley, William. 2022.
"Soil C stock and CO2 production data for Soong et al. 2021: Effects of five years of soil warming at Blodgett Forest, CA.". United States. doi:https://doi.org/10.15485/1896308. https://www.osti.gov/servlets/purl/1896308. Pub date:Sat Jan 01 04:00:00 UTC 2022
@article{osti_1896308,
title = {Soil C stock and CO2 production data for Soong et al. 2021: Effects of five years of soil warming at Blodgett Forest, CA.},
author = {Soong, Jennifer and Hicks Pries, Caitlin and Castanha, Cristina and Porras, Rachel and Ofiti, Nicholas and Torn, Margaret and Schmidt, Michael and Riley, William},
abstractNote = {Subsoils below 20 cm are an important reservoir in the global carbon cycle, but little is known about their vulnerability under climate change. We measured subsoil carbon in warmed vs control plots of a conifer forest after 4.5 years of whole-soil warming (4°C). We also measured soil CO2 efflux at the surface and soil CO2 concentrations along the soil profile. Over the 4.5 years we observed that warming resulted in a loss of subsoil carbon stocks (−33 ± 11%), primarily from unprotected particulate organic matter. Warming also stimulated a sustained 30 ± 4% increase in soil CO2 efflux due to increased CO2 production through the whole-soil profile. The observed in situ decline in subsoil carbon stocks with warming is now definitive evidence of a positive soil carbon-climate feedback, which could not be concluded based on increases in CO2 effluxes alone. This dataset comprises (1) 13C and C recovery in 2014, 2016, and 2018 1m soil cores sampled in 10cm increments. (2) Monthly surface CO2 fluxes from 2014 to 2018. (3) Monthly gas well sample [CO2] and production data. And (4) density fraction data for three depths of cores recovered in 2017.},
doi = {10.15485/1896308},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Sat Jan 01 04:00:00 UTC 2022},
month = {Sat Jan 01 04:00:00 UTC 2022}
}
