Amorphous silica reduces N2O emissions from arable land at the field plot scale
preprint
OA: closed
CC-BY-4.0
Abstract
Abstract Increasing greenhouse gas emissions pose a strong threat due to accelerating global warming. N2O emissions are highly important in this regard as N2O is a very powerful greenhouse gas. Agriculture is the main human-induced source for N2O emissions contributing roughly 60% to total N2O emissions. Soil amorphous silica (ASi) contents are reduced in arable soils due to yearly exports by crop harvest as most crops are silicon accumulator plants. Most recently it has been shown that ASi is increasing water and nutrient availability in soils. Both factors are known to directly and indirectly affect N2O emissions from agroecosystems. In this study we conducted a field plot trial on arable soil depleted in ASi and fertilized this soil its pre-agricultural ASi level. Our data clearly shows that increasing soil ASi to a pre-agricultural level decreased seasonal N2O emissions by ~ 30%. This reduction of N2O emissions due to ASi might be of global relevance as agricultural practice has reduced the ASi content in agricultural soils. If future studies confirm the effect of ASi on N2O emissions, the soil ASi depletion by agricultural practice in the last decades may have led to a substantial increases of N2O emissions.
My notes (saved in your browser only)
Citation neighborhood (no data yet)
We don't have any in-corpus citations linked to this paper yet. This is a recent paper (2024) — citers typically take a year or two to land, and the OpenAlex reference graph may still be filling in.
References (44)
- doi:10.1007/bf00002772 via crossref
- doi:10.1890/06-2057.1 via crossref
- doi:10.1038/472159a via crossref
- doi:10.1098/rstb.2013.0120 via crossref
- doi:10.5194/soil-1-235-2015 via crossref
- doi:10.1016/0038-0717(86)90076-3 via crossref
- doi:10.1016/j.scitotenv.2018.12.100 via crossref
- doi:10.1016/0306-2619(93)90018-k via crossref
- doi:10.1126/science.1176985 via crossref
- doi:10.1038/nclimate1458 via crossref
- doi:10.1371/journal.pone.0129487 via crossref
- doi:10.1088/1748-9326/11/9/095007 via crossref
- doi:10.1016/j.agee.2019.106687 via crossref
- doi:10.1098/rstb.2013.0122 via crossref
- doi:10.1038/s41598-020-59437-x via crossref
- doi:10.3389/fenvs.2020.00094 via crossref
- doi:10.1038/s41598-021-00464-7 via crossref
- doi:10.3390/plants10020295 via crossref
- doi:10.3390/plants10040652 via crossref
- doi:10.1016/j.geoderma.2021.115187 via crossref
- doi:10.1038/s41598-017-09130-3 via crossref
- doi:10.1111/j.1365-2389.2007.00949.x via crossref
- doi:10.5194/bg-8-2281-2011 via crossref
- doi:10.2134/agronj1995.00021962008700060007x via crossref
- doi:10.2136/vzj2019.02.0021 via crossref
- doi:10.1111/ejss.12533 via crossref
- doi:10.1146/annurev-ecolsys-110617-062614 via crossref
- doi:10.1038/s41598-018-37104-6 via crossref
- doi:10.1038/s41598-022-20805-4 via crossref
- doi:10.1016/s1161-0301(98)00019-7 via crossref
- doi:10.1111/j.1365-2389.1991.tb00413.x via crossref
- doi:10.1038/s41598-024-60947-1 via crossref
- doi:10.1016/j.scitotenv.2023.163986 via crossref
- doi:10.1890/08-1122.1 via crossref
- doi:10.1111/gcb.14908 via crossref
- doi:10.1002/1522-2624(200208)165:4<382::aid-jpln382>3.0.co;2-# via crossref
- doi:10.1007/s11104-023-05979-8 via crossref
- doi:10.1111/pce.14858 via crossref
- doi:10.2136/sssaj2004.1295 via crossref
- doi:10.1002/jpln.201600299 via crossref
- doi:10.1002/jeq2.20126 via crossref
- doi:10.1038/srep15912 via crossref
- doi:10.2134/jeq1997.00472425002600020030x via crossref
- doi:10.1016/j.agrformet.2016.03.022 via crossref
Source provenance
- crossref
- last seen: 2026-05-20T01:00:10.111549+00:00
- europepmc
- last seen: 2026-05-20T01:45:00.602351+00:00
- unpaywall
- last seen: 2026-08-19T06:23:00.919175+00:00
License: CC-BY-4.0