Seasonal variability of microbial biomass associated with aggregates in a rice-based ecosystem

Temporal variability of soil microbial biomass shows contradictory trends for different ecosystems. Since soils are comprised of many sizes of aggregates and soil particles, we hypothesized that the microbial biomass response to seasonal variation is more sensitive at the aggregate scale than for wh...

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Published inEuropean journal of soil biology Vol. 56; pp. 84 - 88
Main Authors Jiang, Xianjun, Shi, Xiuli, Wright, Alan L.
Format Journal Article
LanguageEnglish
Published Paris Elsevier Masson SAS 01.05.2013
Elsevier
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Abstract Temporal variability of soil microbial biomass shows contradictory trends for different ecosystems. Since soils are comprised of many sizes of aggregates and soil particles, we hypothesized that the microbial biomass response to seasonal variation is more sensitive at the aggregate scale than for whole soil. Tillage impacts on seasonal variation of microbial biomass were determined for a hydargric Anthrosol in China from 2008 to 2009. No significant seasonal changes occurred for soil total organic C (TOC), but microbial biomass C (MBC) exhibited distinct seasonal variation. However, seasonal variation patterns of MBC associated with aggregates coincided with patterns for whole soil, regardless of tillage regimes. The MBC in whole soil was significantly higher in spring (272 mg kg−1) than autumn (186 mg kg−1) and winter (165 mg kg−1) under CT (conventional tillage), while MBC was higher in spring and autumn than winter and summer for RNT (ridge with no-till). Microorganisms associated with different sizes of aggregates responded similarly to environmental changes, but the degree of response for different sizes of aggregates varied. The CV (coefficient of variation) for seasonal change was lowest for macroaggregates, while the highest CVs occurred for the silt + clay fraction. The results indicated that soil microorganisms associated with macroaggregates were more stable than with silt + clay fractions to resist seasonal changes in climate and soil properties, and therefore more likely to play a role in enhancing nutrient conservation in the soil. Seasonal variation patterns of microbial biomass associated with aggregates coincided with patterns for whole soil, suggesting that microorganisms associated with different size fractions of aggregates respond to macro- and micro-environmental changes in a similar way. •Seasonal patterns of microbial biomass within aggregates were consistent with the whole soil.•Microorganisms associated with macro-aggregates were more resistant to seasonal changes.•Tillage did not increase the seasonal variability of microbial biomass.
AbstractList Temporal variability of soil microbial biomass shows contradictory trends for different ecosystems. Since soils are comprised of many sizes of aggregates and soil particles, we hypothesized that the microbial biomass response to seasonal variation is more sensitive at the aggregate scale than for whole soil. Tillage impacts on seasonal variation of microbial biomass were determined for a hydargric Anthrosol in China from 2008 to 2009. No significant seasonal changes occurred for soil total organic C (TOC), but microbial biomass C (MBC) exhibited distinct seasonal variation. However, seasonal variation patterns of MBC associated with aggregates coincided with patterns for whole soil, regardless of tillage regimes. The MBC in whole soil was significantly higher in spring (272 mg kg⁻¹) than autumn (186 mg kg⁻¹) and winter (165 mg kg⁻¹) under CT (conventional tillage), while MBC was higher in spring and autumn than winter and summer for RNT (ridge with no-till). Microorganisms associated with different sizes of aggregates responded similarly to environmental changes, but the degree of response for different sizes of aggregates varied. The CV (coefficient of variation) for seasonal change was lowest for macroaggregates, while the highest CVs occurred for the silt + clay fraction. The results indicated that soil microorganisms associated with macroaggregates were more stable than with silt + clay fractions to resist seasonal changes in climate and soil properties, and therefore more likely to play a role in enhancing nutrient conservation in the soil. Seasonal variation patterns of microbial biomass associated with aggregates coincided with patterns for whole soil, suggesting that microorganisms associated with different size fractions of aggregates respond to macro- and micro-environmental changes in a similar way.
Temporal variability of soil microbial biomass shows contradictory trends for different ecosystems. Since soils are comprised of many sizes of aggregates and soil particles, we hypothesized that the microbial biomass response to seasonal variation is more sensitive at the aggregate scale than for whole soil. Tillage impacts on seasonal variation of microbial biomass were determined for a hydargric Anthrosol in China from 2008 to 2009. No significant seasonal changes occurred for soil total organic C (TOC), but microbial biomass C (MBC) exhibited distinct seasonal variation. However, seasonal variation patterns of MBC associated with aggregates coincided with patterns for whole soil, regardless of tillage regimes. The MBC in whole soil was significantly higher in spring (272 mg kg−1) than autumn (186 mg kg−1) and winter (165 mg kg−1) under CT (conventional tillage), while MBC was higher in spring and autumn than winter and summer for RNT (ridge with no-till). Microorganisms associated with different sizes of aggregates responded similarly to environmental changes, but the degree of response for different sizes of aggregates varied. The CV (coefficient of variation) for seasonal change was lowest for macroaggregates, while the highest CVs occurred for the silt + clay fraction. The results indicated that soil microorganisms associated with macroaggregates were more stable than with silt + clay fractions to resist seasonal changes in climate and soil properties, and therefore more likely to play a role in enhancing nutrient conservation in the soil. Seasonal variation patterns of microbial biomass associated with aggregates coincided with patterns for whole soil, suggesting that microorganisms associated with different size fractions of aggregates respond to macro- and micro-environmental changes in a similar way. •Seasonal patterns of microbial biomass within aggregates were consistent with the whole soil.•Microorganisms associated with macro-aggregates were more resistant to seasonal changes.•Tillage did not increase the seasonal variability of microbial biomass.
Author Jiang, Xianjun
Shi, Xiuli
Wright, Alan L.
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Keywords Soil structure
Nutrient cycling
Rice soil
Conservation tillage
Translocation
Monocotyledones
Cultivated soil
Biogeochemical cycle
Microbial biomass
Inorganic element
Paddy soil
Oryza
Gramineae
Seasonal variation
Ecosystem
Angiospermae
Nutrient
Herbaceous plant
Spermatophyta
Soil science
Aggregate
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Snippet Temporal variability of soil microbial biomass shows contradictory trends for different ecosystems. Since soils are comprised of many sizes of aggregates and...
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SubjectTerms Agronomy. Soil science and plant productions
Anthrosols
autumn
Biochemistry and biology
Biological and medical sciences
Chemical, physicochemical, biochemical and biological properties
clay
clay fraction
climate change
Conservation tillage
conventional tillage
Cropping systems. Cultivation. Soil tillage
ecosystems
Fundamental and applied biological sciences. Psychology
General agronomy. Plant production
microbial biomass
Microbiology
no-tillage
Nutrient cycling
Physical properties
Physics, chemistry, biochemistry and biology of agricultural and forest soils
Rice soil
seasonal variation
silt
soil aggregates
Soil erosion, conservation, land management and development
soil heterogeneity
soil microorganisms
Soil science
Soil structure
spring
Structure, texture, density, mechanical behavior. Heat and gas exchanges
summer
winter
Title Seasonal variability of microbial biomass associated with aggregates in a rice-based ecosystem
URI https://dx.doi.org/10.1016/j.ejsobi.2013.03.004
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