Soil organic carbon cycling in response to simulated soil moisture variation under field conditions
Abstract The combination of extended dry periods and high intensity rainfall, common in the southeastern US, leads to greater variability in soil moisture and consequently increases uncertainty to microbial processes pertinent to soil carbon (C) mineralization. However, field-based findings on soil...
Guardado en:
Autores principales: | , , , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2021
|
Materias: | |
Acceso en línea: | https://doaj.org/article/bb2337cca0b046158f96edcc18807d94 |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:bb2337cca0b046158f96edcc18807d94 |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:bb2337cca0b046158f96edcc18807d942021-12-02T15:49:43ZSoil organic carbon cycling in response to simulated soil moisture variation under field conditions10.1038/s41598-021-90359-42045-2322https://doaj.org/article/bb2337cca0b046158f96edcc18807d942021-05-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-90359-4https://doaj.org/toc/2045-2322Abstract The combination of extended dry periods and high intensity rainfall, common in the southeastern US, leads to greater variability in soil moisture and consequently increases uncertainty to microbial processes pertinent to soil carbon (C) mineralization. However, field-based findings on soil moisture sensitivity to soil C cycling are very limited. Therefore, a field experiment was conducted in 2018 and 2019 on a soybean (Glycine max L.) cropland in the southeastern US with three soil moisture treatments: drought (simulated using rainout-shelter from June to October in each year), rainfed (natural precipitation), and irrigated (irrigation and precipitation). Soil respiration was measured weekly from May to November in both years. Soil samples were collected multiple times each year from 0–5, 5–15, and 15–30 cm depths to determine microbial biomass C (MBC), extractable organic C (EOC), hydrolytic enzyme activities, and fungal abundance. The cumulative respiration under drought compared to other treatments was lower by 32% to 33% in 2018 and 38% to 45% in 2019. Increased MBC, EOC, and fungal abundance were observed under drought than other treatments. Specific enzyme activity indicated fewer metabolically active microbes under drought treatment compared to rainfed and irrigated treatments. Also, maintenance of enzyme pool was observed under drought condition. These results provide critical insights on microbial metabolism in response to soil moisture variation and how that influences different pools of soil C under field conditions.Shikha SinghMelanie A. MayesAvat ShekoofaStephanie N. KivlinSangeeta BansalSindhu JagadammaNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-13 (2021) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Medicine R Science Q |
spellingShingle |
Medicine R Science Q Shikha Singh Melanie A. Mayes Avat Shekoofa Stephanie N. Kivlin Sangeeta Bansal Sindhu Jagadamma Soil organic carbon cycling in response to simulated soil moisture variation under field conditions |
description |
Abstract The combination of extended dry periods and high intensity rainfall, common in the southeastern US, leads to greater variability in soil moisture and consequently increases uncertainty to microbial processes pertinent to soil carbon (C) mineralization. However, field-based findings on soil moisture sensitivity to soil C cycling are very limited. Therefore, a field experiment was conducted in 2018 and 2019 on a soybean (Glycine max L.) cropland in the southeastern US with three soil moisture treatments: drought (simulated using rainout-shelter from June to October in each year), rainfed (natural precipitation), and irrigated (irrigation and precipitation). Soil respiration was measured weekly from May to November in both years. Soil samples were collected multiple times each year from 0–5, 5–15, and 15–30 cm depths to determine microbial biomass C (MBC), extractable organic C (EOC), hydrolytic enzyme activities, and fungal abundance. The cumulative respiration under drought compared to other treatments was lower by 32% to 33% in 2018 and 38% to 45% in 2019. Increased MBC, EOC, and fungal abundance were observed under drought than other treatments. Specific enzyme activity indicated fewer metabolically active microbes under drought treatment compared to rainfed and irrigated treatments. Also, maintenance of enzyme pool was observed under drought condition. These results provide critical insights on microbial metabolism in response to soil moisture variation and how that influences different pools of soil C under field conditions. |
format |
article |
author |
Shikha Singh Melanie A. Mayes Avat Shekoofa Stephanie N. Kivlin Sangeeta Bansal Sindhu Jagadamma |
author_facet |
Shikha Singh Melanie A. Mayes Avat Shekoofa Stephanie N. Kivlin Sangeeta Bansal Sindhu Jagadamma |
author_sort |
Shikha Singh |
title |
Soil organic carbon cycling in response to simulated soil moisture variation under field conditions |
title_short |
Soil organic carbon cycling in response to simulated soil moisture variation under field conditions |
title_full |
Soil organic carbon cycling in response to simulated soil moisture variation under field conditions |
title_fullStr |
Soil organic carbon cycling in response to simulated soil moisture variation under field conditions |
title_full_unstemmed |
Soil organic carbon cycling in response to simulated soil moisture variation under field conditions |
title_sort |
soil organic carbon cycling in response to simulated soil moisture variation under field conditions |
publisher |
Nature Portfolio |
publishDate |
2021 |
url |
https://doaj.org/article/bb2337cca0b046158f96edcc18807d94 |
work_keys_str_mv |
AT shikhasingh soilorganiccarboncyclinginresponsetosimulatedsoilmoisturevariationunderfieldconditions AT melanieamayes soilorganiccarboncyclinginresponsetosimulatedsoilmoisturevariationunderfieldconditions AT avatshekoofa soilorganiccarboncyclinginresponsetosimulatedsoilmoisturevariationunderfieldconditions AT stephanienkivlin soilorganiccarboncyclinginresponsetosimulatedsoilmoisturevariationunderfieldconditions AT sangeetabansal soilorganiccarboncyclinginresponsetosimulatedsoilmoisturevariationunderfieldconditions AT sindhujagadamma soilorganiccarboncyclinginresponsetosimulatedsoilmoisturevariationunderfieldconditions |
_version_ |
1718385715168935936 |