Effects of slow and fast pyrolysis biochar on N2O emissions and water availability of two soils with high water-filled pore space

Biochars, depending on the types of feedstocks and technological conditions of pyrolysis, can vary significantly in their properties and, therefore, it is difficult to predict biochar-induced effects on nitrous oxide (N2O) emissions from various soils, their physical properties and water availabilit...

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Main Authors: Balashov Eugene, Buchkina Natalya, Šimanský Vladimir, Horák Ján
Format: Article
Language:English
Published: Sciendo 2021-12-01
Series:Journal of Hydrology and Hydromechanics
Subjects:
Online Access:https://doi.org/10.2478/johh-2021-0024
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author Balashov Eugene
Buchkina Natalya
Šimanský Vladimir
Horák Ján
author_facet Balashov Eugene
Buchkina Natalya
Šimanský Vladimir
Horák Ján
author_sort Balashov Eugene
collection DOAJ
description Biochars, depending on the types of feedstocks and technological conditions of pyrolysis, can vary significantly in their properties and, therefore, it is difficult to predict biochar-induced effects on nitrous oxide (N2O) emissions from various soils, their physical properties and water availability. The objectives of this study were (1) to quantify effects of slow pyrolysis biochar (BC) and fast pyrolysis biochar (PYRO) on physical and hydro-physical properties of sandy soil (Haplic Arenosol) and clayey loam soil (Gleyic Fluvisol), and (2) to assess corresponding N2O emissions from these two soils. The study included a 63-day long laboratory investigation. Two doses of BC or PYRO (15 t ha−1 and 30 t ha−1) were applied to the soils in combination or without nitrogen fertilizer (NH4NO3, 90 kg N ha−1). The obtained results have shown a significant decrease in the bulk density of sandy soil after it was amended with either rate of BC or PYRO. Water retention capacity of the soils in all the treatments with BC or PYRO increased considerably although no changes was found in the soil water-filled pore space (WFPS) which was higher than 60%. BC was increasing N2O emission rates from the sandy soil treated with N fertilizer, and reducing N2O emission rates from the clayey loam soil treated with N fertilizer. PYRO was more efficient and was reducing N2O emissions from both fertilized soils, but for the sandy soil the reduction was statistically significant only at higher dose (30 t ha−1) of the biochar.
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spelling doaj.art-640832d03c94449dadbd662aeec1a4a82022-12-21T17:57:39ZengSciendoJournal of Hydrology and Hydromechanics1338-43332021-12-0169446747410.2478/johh-2021-0024Effects of slow and fast pyrolysis biochar on N2O emissions and water availability of two soils with high water-filled pore spaceBalashov Eugene0Buchkina Natalya1Šimanský Vladimir2Horák Ján3Department of Soil Physics, Physical Chemistry and Biophysics, Agrophysical Research Institute, Grazhdansky pr. 14, 195220 St. Petersburg, Russia.Department of Soil Physics, Physical Chemistry and Biophysics, Agrophysical Research Institute, Grazhdansky pr. 14, 195220 St. Petersburg, Russia.Department of Soil Science, Institute of Agronomic Sciences, Faculty of Agrobiology and Food Resources, Slovak University of Agriculture, Tr. A. Hlinku 2, 94901Nitra, Slovakia.Institute of Landscape Engineering, Faculty of Horticulture and Landscape Engineering, Slovak University of Agriculture, Hospodárska 7, 94976Nitra, Slovakia.Biochars, depending on the types of feedstocks and technological conditions of pyrolysis, can vary significantly in their properties and, therefore, it is difficult to predict biochar-induced effects on nitrous oxide (N2O) emissions from various soils, their physical properties and water availability. The objectives of this study were (1) to quantify effects of slow pyrolysis biochar (BC) and fast pyrolysis biochar (PYRO) on physical and hydro-physical properties of sandy soil (Haplic Arenosol) and clayey loam soil (Gleyic Fluvisol), and (2) to assess corresponding N2O emissions from these two soils. The study included a 63-day long laboratory investigation. Two doses of BC or PYRO (15 t ha−1 and 30 t ha−1) were applied to the soils in combination or without nitrogen fertilizer (NH4NO3, 90 kg N ha−1). The obtained results have shown a significant decrease in the bulk density of sandy soil after it was amended with either rate of BC or PYRO. Water retention capacity of the soils in all the treatments with BC or PYRO increased considerably although no changes was found in the soil water-filled pore space (WFPS) which was higher than 60%. BC was increasing N2O emission rates from the sandy soil treated with N fertilizer, and reducing N2O emission rates from the clayey loam soil treated with N fertilizer. PYRO was more efficient and was reducing N2O emissions from both fertilized soils, but for the sandy soil the reduction was statistically significant only at higher dose (30 t ha−1) of the biochar.https://doi.org/10.2478/johh-2021-0024biocharsandy soilclayey loam soilbulk densitywater retention capacityn2o emission
spellingShingle Balashov Eugene
Buchkina Natalya
Šimanský Vladimir
Horák Ján
Effects of slow and fast pyrolysis biochar on N2O emissions and water availability of two soils with high water-filled pore space
Journal of Hydrology and Hydromechanics
biochar
sandy soil
clayey loam soil
bulk density
water retention capacity
n2o emission
title Effects of slow and fast pyrolysis biochar on N2O emissions and water availability of two soils with high water-filled pore space
title_full Effects of slow and fast pyrolysis biochar on N2O emissions and water availability of two soils with high water-filled pore space
title_fullStr Effects of slow and fast pyrolysis biochar on N2O emissions and water availability of two soils with high water-filled pore space
title_full_unstemmed Effects of slow and fast pyrolysis biochar on N2O emissions and water availability of two soils with high water-filled pore space
title_short Effects of slow and fast pyrolysis biochar on N2O emissions and water availability of two soils with high water-filled pore space
title_sort effects of slow and fast pyrolysis biochar on n2o emissions and water availability of two soils with high water filled pore space
topic biochar
sandy soil
clayey loam soil
bulk density
water retention capacity
n2o emission
url https://doi.org/10.2478/johh-2021-0024
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