The Role of Different Earthworm Species (Metaphire Hilgendorfi and Eisenia Fetida) on CO2 Emissions and Microbial Biomass during Barley Decomposition
Earthworms are commonly known as essential modifiers of soil carbon (C) and nitrogen (N) cycles, but the effects of their species on nutrient cycles and interaction with soil microbial activities during the decomposition of organic materials remain unclear. We conducted an incubation experiment to i...
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description | Earthworms are commonly known as essential modifiers of soil carbon (C) and nitrogen (N) cycles, but the effects of their species on nutrient cycles and interaction with soil microbial activities during the decomposition of organic materials remain unclear. We conducted an incubation experiment to investigate the effect of two different epigeic earthworms (M. hilgendorfi and E. fetida) on C and N concentrations and related enzyme activities in agricultural soils with added barley residues (ground barley powder). To achieve this, four treatments were included; (1) M. hilgendorfi and barley, (2) E. fetida and barley, (3) barley without earthworms, and (4) without earthworms and without barley. After 32 days incubation, we measured soil pH, inorganic N, microbial biomass C (MBC), water or hot-water soluble C, and soil enzyme activities. We also measured CO2 emissions during the incubation. Our results indicated the earthworm activity in soils had no effect on the cumulative CO2 emissions. However, M. hilgendorfi had a potential to accumulate MBC (2.9 g kg−1 soil) and nitrate-N (39 mg kg−1 soil), compared to E. fetida (2.5 g kg−1 soil and 14 mg kg−1 soil, respectively). In conclusion, the interaction between soil microbes and earthworm is influenced by earthworm species, consequently influencing the soil C and N dynamics. |
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We conducted an incubation experiment to investigate the effect of two different epigeic earthworms (M. hilgendorfi and E. fetida) on C and N concentrations and related enzyme activities in agricultural soils with added barley residues (ground barley powder). To achieve this, four treatments were included; (1) M. hilgendorfi and barley, (2) E. fetida and barley, (3) barley without earthworms, and (4) without earthworms and without barley. After 32 days incubation, we measured soil pH, inorganic N, microbial biomass C (MBC), water or hot-water soluble C, and soil enzyme activities. We also measured CO2 emissions during the incubation. Our results indicated the earthworm activity in soils had no effect on the cumulative CO2 emissions. However, M. hilgendorfi had a potential to accumulate MBC (2.9 g kg−1 soil) and nitrate-N (39 mg kg−1 soil), compared to E. fetida (2.5 g kg−1 soil and 14 mg kg−1 soil, respectively). In conclusion, the interaction between soil microbes and earthworm is influenced by earthworm species, consequently influencing the soil C and N dynamics.</description><identifier>ISSN: 2071-1050</identifier><identifier>EISSN: 2071-1050</identifier><identifier>DOI: 10.3390/su11236544</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Agricultural land ; Agricultural production ; Barley ; Biomass ; Carbon dioxide ; Decomposition ; Emission measurements ; Emissions ; Enzymatic activity ; Enzymes ; Gram-negative bacteria ; Microorganisms ; Nitrogen ; Nutrient cycles ; Oligochaeta ; Organic materials ; Soil dynamics ; Soil microorganisms ; Soil pH ; Soil water ; Soils ; Worms</subject><ispartof>Sustainability, 2019-11, Vol.11 (23), p.6544</ispartof><rights>2019 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/). 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We conducted an incubation experiment to investigate the effect of two different epigeic earthworms (M. hilgendorfi and E. fetida) on C and N concentrations and related enzyme activities in agricultural soils with added barley residues (ground barley powder). To achieve this, four treatments were included; (1) M. hilgendorfi and barley, (2) E. fetida and barley, (3) barley without earthworms, and (4) without earthworms and without barley. After 32 days incubation, we measured soil pH, inorganic N, microbial biomass C (MBC), water or hot-water soluble C, and soil enzyme activities. We also measured CO2 emissions during the incubation. Our results indicated the earthworm activity in soils had no effect on the cumulative CO2 emissions. However, M. hilgendorfi had a potential to accumulate MBC (2.9 g kg−1 soil) and nitrate-N (39 mg kg−1 soil), compared to E. fetida (2.5 g kg−1 soil and 14 mg kg−1 soil, respectively). In conclusion, the interaction between soil microbes and earthworm is influenced by earthworm species, consequently influencing the soil C and N dynamics.</description><subject>Agricultural land</subject><subject>Agricultural production</subject><subject>Barley</subject><subject>Biomass</subject><subject>Carbon dioxide</subject><subject>Decomposition</subject><subject>Emission measurements</subject><subject>Emissions</subject><subject>Enzymatic activity</subject><subject>Enzymes</subject><subject>Gram-negative bacteria</subject><subject>Microorganisms</subject><subject>Nitrogen</subject><subject>Nutrient cycles</subject><subject>Oligochaeta</subject><subject>Organic materials</subject><subject>Soil dynamics</subject><subject>Soil microorganisms</subject><subject>Soil pH</subject><subject>Soil water</subject><subject>Soils</subject><subject>Worms</subject><issn>2071-1050</issn><issn>2071-1050</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNpNkN1Kw0AQhYMoWLQ3PsGANypE9y9_l7ZNrdBS0HodNptJuyXJxt0E6YP4vkYr6NycufjODOd43hUl95wn5MH1lDIeBkKceCNGIupTEpDTf_u5N3ZuT4bhnCY0HHmfmx3Ci6kQTAkzXZZosekglbbbfRhbw2uLSqODmxV2st1pi7DQ1RabwthSg2wKSLXDRkuYY6cLeQumgemaQVpr57Rp3A-00sqaXMsKJtrU0jkoequbLUykrfAAM1Smbo3T3WC59M5KWTkc_-qF9zZPN9OFv1w_PU8fl74SJOh8QXJKiyKiNFeREjHGTJE4YbQIuWKKomQiyQPGkEQ85iIJg0CwnHLFkRGh-IV3fbzbWvPeo-uyveltM7zMWMA5F5QF4UDdHakhgXMWy6y1upb2kFGSfTef_TXPvwD05XVe</recordid><startdate>20191120</startdate><enddate>20191120</enddate><creator>Hamamoto, Toru</creator><creator>Uchida, Yoshitaka</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>4U-</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><orcidid>https://orcid.org/0000-0003-4354-7842</orcidid><orcidid>https://orcid.org/0000-0002-9954-001X</orcidid></search><sort><creationdate>20191120</creationdate><title>The Role of Different Earthworm Species (Metaphire Hilgendorfi and Eisenia Fetida) on CO2 Emissions and Microbial Biomass during Barley Decomposition</title><author>Hamamoto, Toru ; Uchida, Yoshitaka</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c405t-40b11dd711bc7c48e82c08921d63c2c1ea249b522e073834965542b13c3e204c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Agricultural land</topic><topic>Agricultural production</topic><topic>Barley</topic><topic>Biomass</topic><topic>Carbon dioxide</topic><topic>Decomposition</topic><topic>Emission measurements</topic><topic>Emissions</topic><topic>Enzymatic activity</topic><topic>Enzymes</topic><topic>Gram-negative bacteria</topic><topic>Microorganisms</topic><topic>Nitrogen</topic><topic>Nutrient cycles</topic><topic>Oligochaeta</topic><topic>Organic materials</topic><topic>Soil dynamics</topic><topic>Soil microorganisms</topic><topic>Soil pH</topic><topic>Soil water</topic><topic>Soils</topic><topic>Worms</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Hamamoto, Toru</creatorcontrib><creatorcontrib>Uchida, Yoshitaka</creatorcontrib><collection>CrossRef</collection><collection>University Readers</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><jtitle>Sustainability</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Hamamoto, Toru</au><au>Uchida, Yoshitaka</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Role of Different Earthworm Species (Metaphire Hilgendorfi and Eisenia Fetida) on CO2 Emissions and Microbial Biomass during Barley Decomposition</atitle><jtitle>Sustainability</jtitle><date>2019-11-20</date><risdate>2019</risdate><volume>11</volume><issue>23</issue><spage>6544</spage><pages>6544-</pages><issn>2071-1050</issn><eissn>2071-1050</eissn><abstract>Earthworms are commonly known as essential modifiers of soil carbon (C) and nitrogen (N) cycles, but the effects of their species on nutrient cycles and interaction with soil microbial activities during the decomposition of organic materials remain unclear. We conducted an incubation experiment to investigate the effect of two different epigeic earthworms (M. hilgendorfi and E. fetida) on C and N concentrations and related enzyme activities in agricultural soils with added barley residues (ground barley powder). To achieve this, four treatments were included; (1) M. hilgendorfi and barley, (2) E. fetida and barley, (3) barley without earthworms, and (4) without earthworms and without barley. After 32 days incubation, we measured soil pH, inorganic N, microbial biomass C (MBC), water or hot-water soluble C, and soil enzyme activities. We also measured CO2 emissions during the incubation. Our results indicated the earthworm activity in soils had no effect on the cumulative CO2 emissions. However, M. hilgendorfi had a potential to accumulate MBC (2.9 g kg−1 soil) and nitrate-N (39 mg kg−1 soil), compared to E. fetida (2.5 g kg−1 soil and 14 mg kg−1 soil, respectively). In conclusion, the interaction between soil microbes and earthworm is influenced by earthworm species, consequently influencing the soil C and N dynamics.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/su11236544</doi><orcidid>https://orcid.org/0000-0003-4354-7842</orcidid><orcidid>https://orcid.org/0000-0002-9954-001X</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Agricultural land Agricultural production Barley Biomass Carbon dioxide Decomposition Emission measurements Emissions Enzymatic activity Enzymes Gram-negative bacteria Microorganisms Nitrogen Nutrient cycles Oligochaeta Organic materials Soil dynamics Soil microorganisms Soil pH Soil water Soils Worms |
title | The Role of Different Earthworm Species (Metaphire Hilgendorfi and Eisenia Fetida) on CO2 Emissions and Microbial Biomass during Barley Decomposition |
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