Global N2O emissions from our planet: Which fluxes are affected by man, and can we reduce these?

Research output: Contribution to journal › Review › Research › peer-review

Standard

Global N2O emissions from our planet : Which fluxes are affected by man, and can we reduce these? / Christensen, Søren; Rousk, Kathrin.

In: iScience, Vol. 27, No. 2, 109042, 2024.

Research output: Contribution to journal › Review › Research › peer-review

Harvard

Christensen, S & Rousk, K 2024, 'Global N2O emissions from our planet: Which fluxes are affected by man, and can we reduce these?', iScience, vol. 27, no. 2, 109042. https://doi.org/10.1016/j.isci.2024.109042

APA

Christensen, S., & Rousk, K. (2024). Global N2O emissions from our planet: Which fluxes are affected by man, and can we reduce these? iScience, 27(2), [109042]. https://doi.org/10.1016/j.isci.2024.109042

Vancouver

Christensen S, Rousk K. Global N2O emissions from our planet: Which fluxes are affected by man, and can we reduce these? iScience. 2024;27(2). 109042. https://doi.org/10.1016/j.isci.2024.109042

Author

Christensen, Søren ; Rousk, Kathrin. / Global N2O emissions from our planet : Which fluxes are affected by man, and can we reduce these?. In: iScience. 2024 ; Vol. 27, No. 2.

Bibtex

@article{b24311c38c5847a091ef75cbdddb5f11,
title = "Global N2O emissions from our planet: Which fluxes are affected by man, and can we reduce these?",
abstract = "In some places, N2O emissions have doubled during the last 2-3 decades. Therefore, it is crucial to identify N2O emission hotspots from terrestrial and aquatic systems. Large variation in N2O emissions occur in managed as well as in natural areas. Natural unmanaged tropical and subtropical wet forests are important N2O sources globally. Emission hotspots, often coupled to human activities, vary across climate zones, whereas N2O emissions are most often a few kg N ha−1 year−1 from arable soils, drained organic soils in the boreal and temperate zones often release 20–30 kg N ha−1 year−1. Similar high N2O emissions occur from some tropical crops like tea, palm oil and bamboo. This strong link between increased N2O emissions and human activities highlight the potential to mitigate large emissions. In contrast, water where oxic and anoxic conditions meet are N2O emission hotspots as well, but not possible to reduce.",
author = "S{\o}ren Christensen and Kathrin Rousk",
year = "2024",
doi = "10.1016/j.isci.2024.109042",
language = "English",
volume = "27",
journal = "iScience",
issn = "2589-0042",
publisher = "Elsevier",
number = "2",

}

RIS

TY - JOUR

T1 - Global N2O emissions from our planet

T2 - Which fluxes are affected by man, and can we reduce these?

AU - Christensen, Søren

AU - Rousk, Kathrin

PY - 2024

Y1 - 2024

N2 - In some places, N2O emissions have doubled during the last 2-3 decades. Therefore, it is crucial to identify N2O emission hotspots from terrestrial and aquatic systems. Large variation in N2O emissions occur in managed as well as in natural areas. Natural unmanaged tropical and subtropical wet forests are important N2O sources globally. Emission hotspots, often coupled to human activities, vary across climate zones, whereas N2O emissions are most often a few kg N ha−1 year−1 from arable soils, drained organic soils in the boreal and temperate zones often release 20–30 kg N ha−1 year−1. Similar high N2O emissions occur from some tropical crops like tea, palm oil and bamboo. This strong link between increased N2O emissions and human activities highlight the potential to mitigate large emissions. In contrast, water where oxic and anoxic conditions meet are N2O emission hotspots as well, but not possible to reduce.

AB - In some places, N2O emissions have doubled during the last 2-3 decades. Therefore, it is crucial to identify N2O emission hotspots from terrestrial and aquatic systems. Large variation in N2O emissions occur in managed as well as in natural areas. Natural unmanaged tropical and subtropical wet forests are important N2O sources globally. Emission hotspots, often coupled to human activities, vary across climate zones, whereas N2O emissions are most often a few kg N ha−1 year−1 from arable soils, drained organic soils in the boreal and temperate zones often release 20–30 kg N ha−1 year−1. Similar high N2O emissions occur from some tropical crops like tea, palm oil and bamboo. This strong link between increased N2O emissions and human activities highlight the potential to mitigate large emissions. In contrast, water where oxic and anoxic conditions meet are N2O emission hotspots as well, but not possible to reduce.

U2 - 10.1016/j.isci.2024.109042

DO - 10.1016/j.isci.2024.109042

M3 - Review

C2 - 38333714

VL - 27

JO - iScience

JF - iScience

SN - 2589-0042

IS - 2

M1 - 109042

ER -

ID: 380741939