Modeling of calcium dynamics in soil organic layers

Calcium is a major nutrient regulating metabolism in a plant. Deficiency of calcium results in a growth decline of plant tissues. Ca may be lost from forest soils due to acidic atmospheric deposition and tree harvesting. Plant-available calcium compounds are in the soil cation exchange complex and s...

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Main Authors: Yuliya Sergeevna Khoraskina, Aleksandr Sergeevich Komarov, Maria G. Bezrukova, Miglena K. Zhiyanski
Format: Article
Language:Russian
Published: Institute of Computer Science 2010-03-01
Series:Компьютерные исследования и моделирование
Subjects:
Online Access:http://crm.ics.org.ru/uploads/crm/crm2010-1/crm10112.pdf
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spelling doaj-d6579c65ab484972a2dbbe1919ff08dc2020-11-24T20:53:56ZrusInstitute of Computer ScienceКомпьютерные исследования и моделирование2076-76332077-68532010-03-012110311010.20537/2076-7633-2010-2-1-103-1101655Modeling of calcium dynamics in soil organic layersYuliya Sergeevna KhoraskinaAleksandr Sergeevich KomarovMaria G. BezrukovaMiglena K. ZhiyanskiCalcium is a major nutrient regulating metabolism in a plant. Deficiency of calcium results in a growth decline of plant tissues. Ca may be lost from forest soils due to acidic atmospheric deposition and tree harvesting. Plant-available calcium compounds are in the soil cation exchange complex and soil waters. Model of soil calcium dynamics linking it with the model of soil organic matter dynamics ROMUL in forest ecosystems is developed. ROMUL describes the mineralization and humification of the fraction of fresh litter which is further transformed into complex of partially humified substance (CHS) and then to stable humus (H) in dependence on temperature, soil moisture and chemical composition of the fraction (nitrogen, lignin and ash contents, pH). Rates of decomposition and humification being coefficients in the system of ordinary differential equations are evaluated using laboratory experiments and verified on a set of field experiments. Model of soil calcium dynamics describes calcium flows between pools of soil organic matter. Outputs are plant nutrition, leaching, synthesis of secondary minerals. The model describes transformation and mineralization of forest floor in detail. Experimental data for calibration model was used from spruсe forest of Bulgaria.http://crm.ics.org.ru/uploads/crm/crm2010-1/crm10112.pdfcalcium turnovermathematical modeling of ecosystemssecondary minerals
collection DOAJ
language Russian
format Article
sources DOAJ
author Yuliya Sergeevna Khoraskina
Aleksandr Sergeevich Komarov
Maria G. Bezrukova
Miglena K. Zhiyanski
spellingShingle Yuliya Sergeevna Khoraskina
Aleksandr Sergeevich Komarov
Maria G. Bezrukova
Miglena K. Zhiyanski
Modeling of calcium dynamics in soil organic layers
Компьютерные исследования и моделирование
calcium turnover
mathematical modeling of ecosystems
secondary minerals
author_facet Yuliya Sergeevna Khoraskina
Aleksandr Sergeevich Komarov
Maria G. Bezrukova
Miglena K. Zhiyanski
author_sort Yuliya Sergeevna Khoraskina
title Modeling of calcium dynamics in soil organic layers
title_short Modeling of calcium dynamics in soil organic layers
title_full Modeling of calcium dynamics in soil organic layers
title_fullStr Modeling of calcium dynamics in soil organic layers
title_full_unstemmed Modeling of calcium dynamics in soil organic layers
title_sort modeling of calcium dynamics in soil organic layers
publisher Institute of Computer Science
series Компьютерные исследования и моделирование
issn 2076-7633
2077-6853
publishDate 2010-03-01
description Calcium is a major nutrient regulating metabolism in a plant. Deficiency of calcium results in a growth decline of plant tissues. Ca may be lost from forest soils due to acidic atmospheric deposition and tree harvesting. Plant-available calcium compounds are in the soil cation exchange complex and soil waters. Model of soil calcium dynamics linking it with the model of soil organic matter dynamics ROMUL in forest ecosystems is developed. ROMUL describes the mineralization and humification of the fraction of fresh litter which is further transformed into complex of partially humified substance (CHS) and then to stable humus (H) in dependence on temperature, soil moisture and chemical composition of the fraction (nitrogen, lignin and ash contents, pH). Rates of decomposition and humification being coefficients in the system of ordinary differential equations are evaluated using laboratory experiments and verified on a set of field experiments. Model of soil calcium dynamics describes calcium flows between pools of soil organic matter. Outputs are plant nutrition, leaching, synthesis of secondary minerals. The model describes transformation and mineralization of forest floor in detail. Experimental data for calibration model was used from spruсe forest of Bulgaria.
topic calcium turnover
mathematical modeling of ecosystems
secondary minerals
url http://crm.ics.org.ru/uploads/crm/crm2010-1/crm10112.pdf
work_keys_str_mv AT yuliyasergeevnakhoraskina modelingofcalciumdynamicsinsoilorganiclayers
AT aleksandrsergeevichkomarov modelingofcalciumdynamicsinsoilorganiclayers
AT mariagbezrukova modelingofcalciumdynamicsinsoilorganiclayers
AT miglenakzhiyanski modelingofcalciumdynamicsinsoilorganiclayers
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