Glomalin contribution to soil organic carbon under different pasture managements in a saline soil environment

The glomalin produced by arbuscular mycorrhizal fungi has beneficial effects on soils. We studied the vertical profile of glomalin-related soil protein (GRSP) in pasturelands grown under saline soils and exposed to different management practices. Treatments included haying and grazing of Chloris gay...

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Published inArchiv für Acker- und Pflanzenbau und Bodenkunde Vol. 68; no. 3; pp. 340 - 354
Main Authors Banegas, Natalia, Dos Santos, Daniel Andrés, Guerrero Molina, Fernanda, Albanesi, Ada, Pedraza, Raúl
Format Journal Article
LanguageEnglish
Published Abingdon Taylor & Francis 23.02.2022
Taylor & Francis Ltd
Subjects
Arbuscular mycorrhizas
Biomass
Carbon
carbon sinks
Chloris gayana
Continuity (mathematics)
edaphic factors
Fertilization
glomalin
glomalin-carbon content
Grazing
Nitrogen
Nutrient cycles
Nutrients
Organic carbon
Pasture
Pasture management
pastures
perennial grasses
Saline soils
Soil environment
soil organic carbon
Soil profiles
Soil properties
Spores
total glomalin
total nitrogen
tropical perennial-grasses
vesicular arbuscular mycorrhizae
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Abstract The glomalin produced by arbuscular mycorrhizal fungi has beneficial effects on soils. We studied the vertical profile of glomalin-related soil protein (GRSP) in pasturelands grown under saline soils and exposed to different management practices. Treatments included haying and grazing of Chloris gayana subject to either N-fertilization or not. We measured mycorrhizal colonization, spores, root biomass, total GRSP, GRSP-carbon (GRSP-C), organic carbon (OC) and total nitrogen (TN). In the meanwhile, we also developed a mathematical procedure to fit continuous power functions to binned soil data. Power decay functions adjusted excellently well the measured data across the 1-meter soil profile. Meaningful increases of root biomass, OC, TN, GRSP and GRSP-C values were associated with grazing and fertilization. Particularly, GRSP-C averaged 1,134 kg C ha −1 at the beginning experiments and increased significantly up to 1,261 kg C ha −1 in grazed and fertilized pastures at the end of the study period. Carbon accounted for between 17% and 50% of GRSP, representing in turn 0.52-1.62% of SOC stock. So, a tropical perennial grass can contribute to the carbon stock in saline soils by promoting production of GRSP. This contribution increases when inputs and cycling of nutrients are enhanced (grazing and N-fertilization).
AbstractList The glomalin produced by arbuscular mycorrhizal fungi has beneficial effects on soils. We studied the vertical profile of glomalin-related soil protein (GRSP) in pasturelands grown under saline soils and exposed to different management practices. Treatments included haying and grazing of Chloris gayana subject to either N-fertilization or not. We measured mycorrhizal colonization, spores, root biomass, total GRSP, GRSP-carbon (GRSP-C), organic carbon (OC) and total nitrogen (TN). In the meanwhile, we also developed a mathematical procedure to fit continuous power functions to binned soil data. Power decay functions adjusted excellently well the measured data across the 1-meter soil profile. Meaningful increases of root biomass, OC, TN, GRSP and GRSP-C values were associated with grazing and fertilization. Particularly, GRSP-C averaged 1,134 kg C ha −1 at the beginning experiments and increased significantly up to 1,261 kg C ha −1 in grazed and fertilized pastures at the end of the study period. Carbon accounted for between 17% and 50% of GRSP, representing in turn 0.52-1.62% of SOC stock. So, a tropical perennial grass can contribute to the carbon stock in saline soils by promoting production of GRSP. This contribution increases when inputs and cycling of nutrients are enhanced (grazing and N-fertilization).
The glomalin produced by arbuscular mycorrhizal fungi has beneficial effects on soils. We studied the vertical profile of glomalin-related soil protein (GRSP) in pasturelands grown under saline soils and exposed to different management practices. Treatments included haying and grazing of Chloris gayana subject to either N-fertilization or not. We measured mycorrhizal colonization, spores, root biomass, total GRSP, GRSP-carbon (GRSP-C), organic carbon (OC) and total nitrogen (TN). In the meanwhile, we also developed a mathematical procedure to fit continuous power functions to binned soil data. Power decay functions adjusted excellently well the measured data across the 1-meter soil profile. Meaningful increases of root biomass, OC, TN, GRSP and GRSP-C values were associated with grazing and fertilization. Particularly, GRSP-C averaged 1,134 kg C ha⁻¹ at the beginning experiments and increased significantly up to 1,261 kg C ha⁻¹ in grazed and fertilized pastures at the end of the study period. Carbon accounted for between 17% and 50% of GRSP, representing in turn 0.52–1.62% of SOC stock. So, a tropical perennial grass can contribute to the carbon stock in saline soils by promoting production of GRSP. This contribution increases when inputs and cycling of nutrients are enhanced (grazing and N-fertilization).
The glomalin produced by arbuscular mycorrhizal fungi has beneficial effects on soils. We studied the vertical profile of glomalin-related soil protein (GRSP) in pasturelands grown under saline soils and exposed to different management practices. Treatments included haying and grazing of Chloris gayana subject to either N-fertilization or not. We measured mycorrhizal colonization, spores, root biomass, total GRSP, GRSP-carbon (GRSP-C), organic carbon (OC) and total nitrogen (TN). In the meanwhile, we also developed a mathematical procedure to fit continuous power functions to binned soil data. Power decay functions adjusted excellently well the measured data across the 1-meter soil profile. Meaningful increases of root biomass, OC, TN, GRSP and GRSP-C values were associated with grazing and fertilization. Particularly, GRSP-C averaged 1,134 kg C ha−1 at the beginning experiments and increased significantly up to 1,261 kg C ha−1 in grazed and fertilized pastures at the end of the study period. Carbon accounted for between 17% and 50% of GRSP, representing in turn 0.52–1.62% of SOC stock. So, a tropical perennial grass can contribute to the carbon stock in saline soils by promoting production of GRSP. This contribution increases when inputs and cycling of nutrients are enhanced (grazing and N-fertilization).
Author Pedraza, Raúl
Albanesi, Ada
Dos Santos, Daniel Andrés
Guerrero Molina, Fernanda
Banegas, Natalia
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  givenname: Natalia
  surname: Banegas
  fullname: Banegas, Natalia
  organization: Instituto Nacional de Tecnología Agropecuaria
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  givenname: Daniel Andrés
  surname: Dos Santos
  fullname: Dos Santos, Daniel Andrés
  email: dadossantos@csnat.unt.edu.ar
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  givenname: Fernanda
  surname: Guerrero Molina
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  surname: Albanesi
  fullname: Albanesi, Ada
  organization: Universidad Nacional de Santiago del Estero
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  givenname: Raúl
  surname: Pedraza
  fullname: Pedraza, Raúl
  organization: Universidad Nacional De Tucumán
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Snippet The glomalin produced by arbuscular mycorrhizal fungi has beneficial effects on soils. We studied the vertical profile of glomalin-related soil protein (GRSP)...
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SubjectTerms Arbuscular mycorrhizas
Biomass
Carbon
carbon sinks
Chloris gayana
Continuity (mathematics)
edaphic factors
Fertilization
glomalin
glomalin-carbon content
Grazing
Nitrogen
Nutrient cycles
Nutrients
Organic carbon
Pasture
Pasture management
pastures
perennial grasses
Saline soils
Soil environment
soil organic carbon
Soil profiles
Soil properties
Spores
total glomalin
total nitrogen
tropical perennial-grasses
vesicular arbuscular mycorrhizae
Title Glomalin contribution to soil organic carbon under different pasture managements in a saline soil environment
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