Modeling Chloride Retention in Boreal Forest Soils - synergy of input treatments and microbial biomass

The hypothetical assumption that chloride is conservative in the soil has been debated for the last decade. The results of the recent years of study in chlorine biogeochemistry show that chloride is non-conservative but rather participates in complex biogeochemical reactions in the soil. These inter...

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Main Author: Oni, Stephen Kayode
Format: Others
Language:English
Published: Linköpings universitet, Tema vatten i natur och samhälle 2007
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-9312
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spelling ndltd-UPSALLA1-oai-DiVA.org-liu-93122013-01-08T13:14:48ZModeling Chloride Retention in Boreal Forest Soils - synergy of input treatments and microbial biomassengOni, Stephen KayodeLinköpings universitet, Tema vatten i natur och samhälleTema vatten i natur och samhälle2007Biogeochemical modelChlorine biogeochemistryChlorine cyclesChloride immobilizationMicrobial BiomassWater residence timeEnvironmental chemistryMiljökemiThe hypothetical assumption that chloride is conservative in the soil has been debated for the last decade. The results of the recent years of study in chlorine biogeochemistry show that chloride is non-conservative but rather participates in complex biogeochemical reactions in the soil. These interactions in nature inform the development of simplified hydrochemical model of chloride dynamics in the soil that is driven on soil routine component of HBV hydrological model. This novel attempt affords the opportunity to explore chlorine biogeochemistry further by evaluating the biological processes such as microbial biomass that predominate chlorine cycles in the same order of magnitude as earlier studied abiotic factors. Data from soil lysimeter experiment with different inputs treatments were used in the calibration and validation of both the hydrological and biogeochemical model. The results show that (1) model efficiency reduces with decreasing water residence and with increasing soil organic matter. (2) Longer water residence time (low water input), high chloride and high nitrogen input loads relatively enhance maximum biomass accumulation in a shorter time span. (3) Chloride retention time reduces with increasing chloride loads under short water residence. (4) Microbial biomass growth rate is highest under high chloride input treatments. (5) Biomass death rates shows reducing trend under short water residence (High water input). Further researches are therefore suggested for possible model expansion and to make the results of this model plausible under field conditions. Student thesisinfo:eu-repo/semantics/bachelorThesistexthttp://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-9312application/pdfinfo:eu-repo/semantics/openAccess
collection NDLTD
language English
format Others
sources NDLTD
topic Biogeochemical model
Chlorine biogeochemistry
Chlorine cycles
Chloride immobilization
Microbial Biomass
Water residence time
Environmental chemistry
Miljökemi
spellingShingle Biogeochemical model
Chlorine biogeochemistry
Chlorine cycles
Chloride immobilization
Microbial Biomass
Water residence time
Environmental chemistry
Miljökemi
Oni, Stephen Kayode
Modeling Chloride Retention in Boreal Forest Soils - synergy of input treatments and microbial biomass
description The hypothetical assumption that chloride is conservative in the soil has been debated for the last decade. The results of the recent years of study in chlorine biogeochemistry show that chloride is non-conservative but rather participates in complex biogeochemical reactions in the soil. These interactions in nature inform the development of simplified hydrochemical model of chloride dynamics in the soil that is driven on soil routine component of HBV hydrological model. This novel attempt affords the opportunity to explore chlorine biogeochemistry further by evaluating the biological processes such as microbial biomass that predominate chlorine cycles in the same order of magnitude as earlier studied abiotic factors. Data from soil lysimeter experiment with different inputs treatments were used in the calibration and validation of both the hydrological and biogeochemical model. The results show that (1) model efficiency reduces with decreasing water residence and with increasing soil organic matter. (2) Longer water residence time (low water input), high chloride and high nitrogen input loads relatively enhance maximum biomass accumulation in a shorter time span. (3) Chloride retention time reduces with increasing chloride loads under short water residence. (4) Microbial biomass growth rate is highest under high chloride input treatments. (5) Biomass death rates shows reducing trend under short water residence (High water input). Further researches are therefore suggested for possible model expansion and to make the results of this model plausible under field conditions.
author Oni, Stephen Kayode
author_facet Oni, Stephen Kayode
author_sort Oni, Stephen Kayode
title Modeling Chloride Retention in Boreal Forest Soils - synergy of input treatments and microbial biomass
title_short Modeling Chloride Retention in Boreal Forest Soils - synergy of input treatments and microbial biomass
title_full Modeling Chloride Retention in Boreal Forest Soils - synergy of input treatments and microbial biomass
title_fullStr Modeling Chloride Retention in Boreal Forest Soils - synergy of input treatments and microbial biomass
title_full_unstemmed Modeling Chloride Retention in Boreal Forest Soils - synergy of input treatments and microbial biomass
title_sort modeling chloride retention in boreal forest soils - synergy of input treatments and microbial biomass
publisher Linköpings universitet, Tema vatten i natur och samhälle
publishDate 2007
url http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-9312
work_keys_str_mv AT onistephenkayode modelingchlorideretentioninborealforestsoilssynergyofinputtreatmentsandmicrobialbiomass
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