Abiotic pulses and microbial activity lags in greenhouse gas emissions due to tillage

Abstract Tillage affects atmosphere–soil greenhouse gas (GHG) flux by opening soil pore spaces releasing pockets of CO2, CH4, and N2O. Tillage may also stimulate microbes responsible for GHG biogenesis and consumption at longer time scales following a discrete tillage event. I measured soil gas flux...

Full description

Bibliographic Details
Main Author: Benjamin D. Duval
Format: Article
Language:English
Published: Wiley 2020-01-01
Series:Agrosystems, Geosciences & Environment
Online Access:https://doi.org/10.1002/agg2.20037
id doaj-efc67f46a5484dea9767148dc8f70615
record_format Article
spelling doaj-efc67f46a5484dea9767148dc8f706152021-02-19T11:21:43ZengWileyAgrosystems, Geosciences & Environment2639-66962020-01-0131n/an/a10.1002/agg2.20037Abiotic pulses and microbial activity lags in greenhouse gas emissions due to tillageBenjamin D. Duval0Biology Department New Mexico Institute of Mining and Technology Socorro NM 87801 USAAbstract Tillage affects atmosphere–soil greenhouse gas (GHG) flux by opening soil pore spaces releasing pockets of CO2, CH4, and N2O. Tillage may also stimulate microbes responsible for GHG biogenesis and consumption at longer time scales following a discrete tillage event. I measured soil gas flux immediately after three mechanically different tillage events (moldboard plow, rip‐plow, and disc‐till) over 2 mo within the same field. Delayed effects of tillage on soil respiration were measured; CH4 and N2O fluxes via laboratory incubations on soils were collected following tillage events compared to undisturbed soils. Moldboard plowing did not result in immediate pulses of GHG. Carbon dioxide emissions and CH4 influx to soil peaked 1 h post‐plow. Later rip‐plowing caused a more sustained pulse of CO2 and CH4 uptake over 2 h in the field. Disc‐tillage produced a CO2 production pulse‐then‐decline profile, but CH4 and N2O fluxes were highly variable after this event. Greenhouse gas flux from laboratory‐incubated alfalfa soil and fallow soil were similar to soil collected after rip‐plowing. Soils incubated after the last field tillage event produced significantly lower CO2 emissions during lab incubations compared with other undisturbed and plowed soil. These results show that instantaneous tillage effects are not uniform among GHGs, tillage alteration of soil respiration persists for months following a disturbance, and repeated tillage in the field changes microbial regulation of specific GHGs. Tillage has immediate impacts on GHG flux and has the potential for persistent effects on microbial activity that need further investigation as a GHG abatement tool.https://doi.org/10.1002/agg2.20037
collection DOAJ
language English
format Article
sources DOAJ
author Benjamin D. Duval
spellingShingle Benjamin D. Duval
Abiotic pulses and microbial activity lags in greenhouse gas emissions due to tillage
Agrosystems, Geosciences & Environment
author_facet Benjamin D. Duval
author_sort Benjamin D. Duval
title Abiotic pulses and microbial activity lags in greenhouse gas emissions due to tillage
title_short Abiotic pulses and microbial activity lags in greenhouse gas emissions due to tillage
title_full Abiotic pulses and microbial activity lags in greenhouse gas emissions due to tillage
title_fullStr Abiotic pulses and microbial activity lags in greenhouse gas emissions due to tillage
title_full_unstemmed Abiotic pulses and microbial activity lags in greenhouse gas emissions due to tillage
title_sort abiotic pulses and microbial activity lags in greenhouse gas emissions due to tillage
publisher Wiley
series Agrosystems, Geosciences & Environment
issn 2639-6696
publishDate 2020-01-01
description Abstract Tillage affects atmosphere–soil greenhouse gas (GHG) flux by opening soil pore spaces releasing pockets of CO2, CH4, and N2O. Tillage may also stimulate microbes responsible for GHG biogenesis and consumption at longer time scales following a discrete tillage event. I measured soil gas flux immediately after three mechanically different tillage events (moldboard plow, rip‐plow, and disc‐till) over 2 mo within the same field. Delayed effects of tillage on soil respiration were measured; CH4 and N2O fluxes via laboratory incubations on soils were collected following tillage events compared to undisturbed soils. Moldboard plowing did not result in immediate pulses of GHG. Carbon dioxide emissions and CH4 influx to soil peaked 1 h post‐plow. Later rip‐plowing caused a more sustained pulse of CO2 and CH4 uptake over 2 h in the field. Disc‐tillage produced a CO2 production pulse‐then‐decline profile, but CH4 and N2O fluxes were highly variable after this event. Greenhouse gas flux from laboratory‐incubated alfalfa soil and fallow soil were similar to soil collected after rip‐plowing. Soils incubated after the last field tillage event produced significantly lower CO2 emissions during lab incubations compared with other undisturbed and plowed soil. These results show that instantaneous tillage effects are not uniform among GHGs, tillage alteration of soil respiration persists for months following a disturbance, and repeated tillage in the field changes microbial regulation of specific GHGs. Tillage has immediate impacts on GHG flux and has the potential for persistent effects on microbial activity that need further investigation as a GHG abatement tool.
url https://doi.org/10.1002/agg2.20037
work_keys_str_mv AT benjamindduval abioticpulsesandmicrobialactivitylagsingreenhousegasemissionsduetotillage
_version_ 1724261210502725632