Similar strong impact of N fertilizer form and soil erosion state on N2O emissions from croplands

•Soil erosion states strongly impact N2O emission similar to N fertilizer form.•Organic fertilizer resulted in highest N2O emission compared to mixed and mineral.•Depositional soil resulted in highest N2O emission compared to non-eroded and eroded.•Site-specific differences in soil properties induce...

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Published inGeoderma Vol. 429; p. 116243
Main Authors Vaidya, Shrijana, Hoffmann, Mathias, Holz, Maire, Macagga, Reena, Monzon, Oscar, Thalmann, Mogens, Jurisch, Nicole, Pehle, Natalia, Verch, Gernot, Sommer, Michael, Augustin, Jürgen
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.01.2023
Subjects
Manual chamber
N fertilization form
Nitrous oxide emission
Soil
Soil erosion
N fertilization form
Soil
Soil erosion
Manual chamber
Nitrous oxide emission
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Abstract •Soil erosion states strongly impact N2O emission similar to N fertilizer form.•Organic fertilizer resulted in highest N2O emission compared to mixed and mineral.•Depositional soil resulted in highest N2O emission compared to non-eroded and eroded.•Site-specific differences in soil properties induced by erosion influence N2O emission. Soil erosion affects 20% of croplands worldwide. However, understanding the effect of soil erosion on N2O emissions, which is one of the most potent greenhouse gases, is still limited. This limitation is likely because the small-scale differences in soil properties and fertility induced by erosion (i.e. ranges of erosion states) have barely been considered in studies quantifying N2O emissions from croplands. There are, however, indications that the erosion state itself strongly impacts N2O emission, similar to the N fertilizer form. Therefore, our investigations aimed to further explore these indications. We measured N2O fluxes for three years and at five sites within an erosion affected field experiment. N2O emissions were quantified using a manual chamber system. Three sites were established on a summit position (Albic Luvisol; non-eroded) but differed in N fertilizer forms (organic biogas fermented residues, calcium ammonium nitrate and a mixture of both fertilizers). Two additional sites were established on an extremely eroded soil (Calcaric Regosol) and wet depositional soil in a depression (Endogleyic Colluvic Regosol) to measure the effect of soil erosion states on N2O emissions. Both additional sites were fertilized with calcium ammonium nitrate only. In case of the non-eroded soil (summit), organic fertilization resulted in the highest cumulative N2O emission (6.2 ± 0.21 kg N2O-N/ha y−1) compared to mixed (5.5 ± 0.18 kg N2O-N/ha y−1) and mineral (1.9 ± 0.17 kg N2O-N/ha y−1) fertilization. These high emissions were probably caused by soluble C and N substrates from organic fertilizer, resulting in microbial activities favoring high N2O emissions. Regarding the erosion status, we observed the highest N2O emissions in the depositional soil (2.8 ± 0.21 kg N2O-N/ha y−1), followed by the non-eroded (1.9 ± 0.17 kg N2O-N/ha y−1) and the extremely eroded soil (0.6 ± 0.03 kg N2O-N/ha y−1). These differences in N2O emissions were mainly due to the site-specific, erosion induced differences in soil properties such as soil texture, soil organic C and total N contents and stocks, water-filled pore space and soil pH. These results indicate that soil erosion state may indeed be of similar importance, as N fertilizer form, for the magnitude of N2O emissions from croplands.
AbstractList •Soil erosion states strongly impact N2O emission similar to N fertilizer form.•Organic fertilizer resulted in highest N2O emission compared to mixed and mineral.•Depositional soil resulted in highest N2O emission compared to non-eroded and eroded.•Site-specific differences in soil properties induced by erosion influence N2O emission. Soil erosion affects 20% of croplands worldwide. However, understanding the effect of soil erosion on N2O emissions, which is one of the most potent greenhouse gases, is still limited. This limitation is likely because the small-scale differences in soil properties and fertility induced by erosion (i.e. ranges of erosion states) have barely been considered in studies quantifying N2O emissions from croplands. There are, however, indications that the erosion state itself strongly impacts N2O emission, similar to the N fertilizer form. Therefore, our investigations aimed to further explore these indications. We measured N2O fluxes for three years and at five sites within an erosion affected field experiment. N2O emissions were quantified using a manual chamber system. Three sites were established on a summit position (Albic Luvisol; non-eroded) but differed in N fertilizer forms (organic biogas fermented residues, calcium ammonium nitrate and a mixture of both fertilizers). Two additional sites were established on an extremely eroded soil (Calcaric Regosol) and wet depositional soil in a depression (Endogleyic Colluvic Regosol) to measure the effect of soil erosion states on N2O emissions. Both additional sites were fertilized with calcium ammonium nitrate only. In case of the non-eroded soil (summit), organic fertilization resulted in the highest cumulative N2O emission (6.2 ± 0.21 kg N2O-N/ha y−1) compared to mixed (5.5 ± 0.18 kg N2O-N/ha y−1) and mineral (1.9 ± 0.17 kg N2O-N/ha y−1) fertilization. These high emissions were probably caused by soluble C and N substrates from organic fertilizer, resulting in microbial activities favoring high N2O emissions. Regarding the erosion status, we observed the highest N2O emissions in the depositional soil (2.8 ± 0.21 kg N2O-N/ha y−1), followed by the non-eroded (1.9 ± 0.17 kg N2O-N/ha y−1) and the extremely eroded soil (0.6 ± 0.03 kg N2O-N/ha y−1). These differences in N2O emissions were mainly due to the site-specific, erosion induced differences in soil properties such as soil texture, soil organic C and total N contents and stocks, water-filled pore space and soil pH. These results indicate that soil erosion state may indeed be of similar importance, as N fertilizer form, for the magnitude of N2O emissions from croplands.
ArticleNumber 116243
Author Monzon, Oscar
Jurisch, Nicole
Pehle, Natalia
Thalmann, Mogens
Verch, Gernot
Augustin, Jürgen
Vaidya, Shrijana
Sommer, Michael
Hoffmann, Mathias
Holz, Maire
Macagga, Reena
Author_xml – sequence: 1
  givenname: Shrijana
  surname: Vaidya
  fullname: Vaidya, Shrijana
  email: shrijana.vaidya@zalf.de
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
– sequence: 2
  givenname: Mathias
  surname: Hoffmann
  fullname: Hoffmann, Mathias
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
– sequence: 3
  givenname: Maire
  surname: Holz
  fullname: Holz, Maire
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
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  givenname: Reena
  surname: Macagga
  fullname: Macagga, Reena
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
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  givenname: Oscar
  surname: Monzon
  fullname: Monzon, Oscar
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
– sequence: 6
  givenname: Mogens
  surname: Thalmann
  fullname: Thalmann, Mogens
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
– sequence: 7
  givenname: Nicole
  surname: Jurisch
  fullname: Jurisch, Nicole
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
– sequence: 8
  givenname: Natalia
  surname: Pehle
  fullname: Pehle, Natalia
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
– sequence: 9
  givenname: Gernot
  surname: Verch
  fullname: Verch, Gernot
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Experimental Infrastructure Platform, Steinfurther Straße 14, 17291 Prenzlau, Germany
– sequence: 10
  givenname: Michael
  surname: Sommer
  fullname: Sommer, Michael
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Landscape Pedology, Eberswalder Str. 84, 15374 Müncheberg, Germany
– sequence: 11
  givenname: Jürgen
  surname: Augustin
  fullname: Augustin, Jürgen
  organization: Leibniz Center for Agricultural Landscape Research (ZALF), Working Group for Isotope Biogeochemistry and Gas Fluxes, Eberswalder Str. 84, 15374 Müncheberg, Germany
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Keywords N fertilization form
Soil
Soil erosion
Manual chamber
Nitrous oxide emission
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Snippet •Soil erosion states strongly impact N2O emission similar to N fertilizer form.•Organic fertilizer resulted in highest N2O emission compared to mixed and...
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SubjectTerms Manual chamber
N fertilization form
Nitrous oxide emission
Soil
Soil erosion
Title Similar strong impact of N fertilizer form and soil erosion state on N2O emissions from croplands
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