Impact of Soil Organic Layer Thickness on Soil-to-Atmosphere GHG Fluxes in Grassland in Latvia

Dana Purviņa, Zaiga Anna Zvaigzne, Ilona Skranda, Raitis Normunds Meļņiks, Guna Petaja, Ieva Līcīte, Aldis Butlers and Arta Bārdule ()
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Dana Purviņa: Latvian State Forest Research Institute ‘Silava’, LV-2169 Salaspils, Latvia
Zaiga Anna Zvaigzne: Latvian State Forest Research Institute ‘Silava’, LV-2169 Salaspils, Latvia
Ilona Skranda: Latvian State Forest Research Institute ‘Silava’, LV-2169 Salaspils, Latvia
Raitis Normunds Meļņiks: Latvian State Forest Research Institute ‘Silava’, LV-2169 Salaspils, Latvia
Guna Petaja: Latvian State Forest Research Institute ‘Silava’, LV-2169 Salaspils, Latvia
Ieva Līcīte: Latvian State Forest Research Institute ‘Silava’, LV-2169 Salaspils, Latvia
Aldis Butlers: Latvian State Forest Research Institute ‘Silava’, LV-2169 Salaspils, Latvia
Arta Bārdule: Latvian State Forest Research Institute ‘Silava’, LV-2169 Salaspils, Latvia

Agriculture, 2024, vol. 14, issue 3, 1-18

Abstract: Drained organic soils in agricultural land are considered significant contributors to total greenhouse gas (GHG) emissions, although the temporal and spatial variation of GHG emissions is high. Here, we present results of the study on soil-to-atmosphere fluxes of carbon dioxide (CO 2 ), nitrous oxide (N 2 O) and methane (CH 4 ) from drained organic (fen) soils in grassland. A two-year study (from July 2021 to June 2023) was conducted in three research sites in Latvia (Europe’s hemiboreal zone). Soil total respiration (R tot ), CH 4 and N 2 O fluxes were determined using a manual opaque chamber technique in combination with gas chromatography, while soil heterotrophic respiration (R het ) was measured with a portable spectrometer. Among research sites, the thickness of the soil organic layer ranged from 10 to 70 cm and mean groundwater level ranged from 27 to 99 cm below the soil surface. Drained organic soil in all research sites was a net source of CO 2 emissions (mean 3.48 ± 0.33 t CO 2 -C ha −1 yr −1 ). No evidence was obtained that the thickness of the soil organic layer (ranging from 10 to 70 cm) and OC stock in soil can be considered one of the main affecting factors of magnitude of net CO 2 emissions from drained organic soil. Drained organic soil in grassland was mostly a source of N 2 O emissions (mean 2.39 ± 0.70 kg N 2 O-N ha −1 yr −1 ), while the soil both emitted and consumed atmospheric CH 4 depending on the thickness of the soil organic layer (ranging from −3.26 ± 1.33 to 0.96 ± 0.10 kg CH 4 -C ha −1 yr −1 ).

Keywords: GHG emissions; organic soil; agricultural land; drained grassland; hemiboreal zone (search for similar items in EconPapers)
JEL-codes: Q1 Q10 Q11 Q12 Q13 Q14 Q15 Q16 Q17 Q18 (search for similar items in EconPapers)
Date: 2024
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