2023
DOI: 10.1016/j.chemer.2023.125989
|View full text |Cite
|
Sign up to set email alerts
|

Temperature and soil moisture control CO2 flux and CH4 oxidation in urban ecosystems

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

0
6
0

Year Published

2024
2024
2024
2024

Publication Types

Select...
3
2

Relationship

0
5

Authors

Journals

citations
Cited by 7 publications
(6 citation statements)
references
References 78 publications
0
6
0
Order By: Relevance
“…The seasonal diurnal courses of CH 4 reproduced a gaussian shape in all seasons in both sites, with the highest emissions peak which moved from early morning in summer and spring, to the afternoon in winter and autumn. This dynamic suggested that the combination of thermal variables and water availability were the main drivers for the methane formation processes [ 52 , 53 ]. Specifically, whilst in summertime the effect of solar radiation on soil CH 4 processes was maximum in the first hours of the morning, when water content was available due to nighttime dew deposition, in autumn and wintertime the solar radiation effect was maximum in the afternoon, when it was able to warm soil and water availability was not a limiting factor.…”
Section: Discussionmentioning
confidence: 99%
“…The seasonal diurnal courses of CH 4 reproduced a gaussian shape in all seasons in both sites, with the highest emissions peak which moved from early morning in summer and spring, to the afternoon in winter and autumn. This dynamic suggested that the combination of thermal variables and water availability were the main drivers for the methane formation processes [ 52 , 53 ]. Specifically, whilst in summertime the effect of solar radiation on soil CH 4 processes was maximum in the first hours of the morning, when water content was available due to nighttime dew deposition, in autumn and wintertime the solar radiation effect was maximum in the afternoon, when it was able to warm soil and water availability was not a limiting factor.…”
Section: Discussionmentioning
confidence: 99%
“…Soil acts as a source of CO2 through biochemical processes related to the activity of microorganisms and plant root respiration, which are mainly influenced by soil temperature and moisture [46][47][48]. The movement of CO2 in the soil and from the soil to the atmosphere is facilitated by diffusion and mass flux, which are influenced by soil texture, structure, and moisture [48][49][50]. It is therefore essential to select and manage agricultural systems in a way that increases soil carbon stocks and reduces CO2 emissions from soils [51][52][53][54].…”
Section: Discussionmentioning
confidence: 99%
“…Soil acts as a source of CO 2 through biochemical processes related to the activity of microorganisms and plant root respiration, which are mainly influenced by soil temperature and moisture [46][47][48]. The movement of CO 2 in the soil and from the soil to the atmosphere is facilitated by diffusion and mass flux, which are influenced by soil texture, structure, and moisture [48][49][50]. Therefore, it is essential to select and manage agricultural systems in a way that increases soil carbon stocks and reduces CO 2 emissions from soils [51][52][53][54].…”
Section: Discussionmentioning
confidence: 99%