Silicon Cycling in Soils Revisited

Silicon (Si) speciation and availability in soils is highly important for ecosystem functioning, because Si is a beneficial element for plant growth. Si chemistry is highly complex compared to other elements in soils, because Si reaction rates are relatively slow and dependent on Si species. Consequ...

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Main Authors: Jörg Schaller, Daniel Puppe, Danuta Kaczorek, Ruth Ellerbrock, Michael Sommer
Format: Article
Language:English
Published: MDPI AG 2021-02-01
Series:Plants
Subjects:
Online Access:https://www.mdpi.com/2223-7747/10/2/295
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author Jörg Schaller
Daniel Puppe
Danuta Kaczorek
Ruth Ellerbrock
Michael Sommer
author_facet Jörg Schaller
Daniel Puppe
Danuta Kaczorek
Ruth Ellerbrock
Michael Sommer
author_sort Jörg Schaller
collection DOAJ
description Silicon (Si) speciation and availability in soils is highly important for ecosystem functioning, because Si is a beneficial element for plant growth. Si chemistry is highly complex compared to other elements in soils, because Si reaction rates are relatively slow and dependent on Si species. Consequently, we review the occurrence of different Si species in soil solution and their changes by polymerization, depolymerization, and condensation in relation to important soil processes. We show that an argumentation based on thermodynamic endmembers of Si dependent processes, as currently done, is often difficult, because some reactions such as mineral crystallization require months to years (sometimes even centuries or millennia). Furthermore, we give an overview of Si reactions in soil solution and the predominance of certain solid compounds, which is a neglected but important parameter controlling the availability, reactivity, and function of Si in soils. We further discuss the drivers of soil Si cycling and how humans interfere with these processes. The soil Si cycle is of major importance for ecosystem functioning; therefore, a deeper understanding of drivers of Si cycling (e.g., predominant speciation), human disturbances and the implication for important soil properties (water storage, nutrient availability, and micro aggregate stability) is of fundamental relevance.
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spelling doaj.art-3646c9d769bf485c8fa6a78863e5cb842023-12-03T12:22:11ZengMDPI AGPlants2223-77472021-02-0110229510.3390/plants10020295Silicon Cycling in Soils RevisitedJörg Schaller0Daniel Puppe1Danuta Kaczorek2Ruth Ellerbrock3Michael Sommer4Leibniz Centre for Agricultural Landscape Research (ZALF), 15374 Müncheberg, GermanyLeibniz Centre for Agricultural Landscape Research (ZALF), 15374 Müncheberg, GermanyLeibniz Centre for Agricultural Landscape Research (ZALF), 15374 Müncheberg, GermanyLeibniz Centre for Agricultural Landscape Research (ZALF), 15374 Müncheberg, GermanyLeibniz Centre for Agricultural Landscape Research (ZALF), 15374 Müncheberg, GermanySilicon (Si) speciation and availability in soils is highly important for ecosystem functioning, because Si is a beneficial element for plant growth. Si chemistry is highly complex compared to other elements in soils, because Si reaction rates are relatively slow and dependent on Si species. Consequently, we review the occurrence of different Si species in soil solution and their changes by polymerization, depolymerization, and condensation in relation to important soil processes. We show that an argumentation based on thermodynamic endmembers of Si dependent processes, as currently done, is often difficult, because some reactions such as mineral crystallization require months to years (sometimes even centuries or millennia). Furthermore, we give an overview of Si reactions in soil solution and the predominance of certain solid compounds, which is a neglected but important parameter controlling the availability, reactivity, and function of Si in soils. We further discuss the drivers of soil Si cycling and how humans interfere with these processes. The soil Si cycle is of major importance for ecosystem functioning; therefore, a deeper understanding of drivers of Si cycling (e.g., predominant speciation), human disturbances and the implication for important soil properties (water storage, nutrient availability, and micro aggregate stability) is of fundamental relevance.https://www.mdpi.com/2223-7747/10/2/295andosolsclay neoformationcrop yieldland use changemicro aggregate stabilityphytoliths
spellingShingle Jörg Schaller
Daniel Puppe
Danuta Kaczorek
Ruth Ellerbrock
Michael Sommer
Silicon Cycling in Soils Revisited
Plants
andosols
clay neoformation
crop yield
land use change
micro aggregate stability
phytoliths
title Silicon Cycling in Soils Revisited
title_full Silicon Cycling in Soils Revisited
title_fullStr Silicon Cycling in Soils Revisited
title_full_unstemmed Silicon Cycling in Soils Revisited
title_short Silicon Cycling in Soils Revisited
title_sort silicon cycling in soils revisited
topic andosols
clay neoformation
crop yield
land use change
micro aggregate stability
phytoliths
url https://www.mdpi.com/2223-7747/10/2/295
work_keys_str_mv AT jorgschaller siliconcyclinginsoilsrevisited
AT danielpuppe siliconcyclinginsoilsrevisited
AT danutakaczorek siliconcyclinginsoilsrevisited
AT ruthellerbrock siliconcyclinginsoilsrevisited
AT michaelsommer siliconcyclinginsoilsrevisited