Microfluidic Leaching of Soil Minerals: Release of K+ from K Feldspar.

The rate of K+ leaching from soil minerals such as K-feldspar is believed to be too slow to provide agronomic benefit. Currently, theories and methods available to interpret kinetics of mineral processes in soil fail to consider its microfluidic nature. In this study, we measure the leaching rate of...

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Main Authors: Davide Ciceri, Antoine Allanore
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2015-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC4613825?pdf=render
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author Davide Ciceri
Antoine Allanore
author_facet Davide Ciceri
Antoine Allanore
author_sort Davide Ciceri
collection DOAJ
description The rate of K+ leaching from soil minerals such as K-feldspar is believed to be too slow to provide agronomic benefit. Currently, theories and methods available to interpret kinetics of mineral processes in soil fail to consider its microfluidic nature. In this study, we measure the leaching rate of K+ ions from a K-feldspar-bearing rock (syenite) in a microfluidic environment, and demonstrate that at the spatial and temporal scales experienced by crop roots, K+ is available at a faster rate than that measured with conventional apparatuses. We present a device to investigate kinetics of mineral leaching at an unprecedented simultaneous resolution of space (~101-102 μm), time (~101-102 min) and fluid volume (~100-101 mL). Results obtained from such a device challenge the notion that silicate minerals cannot be used as alternative fertilizers for tropical soils.
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spelling doaj.art-52855ef2d46e4333b16d040af305ed342022-12-21T19:47:41ZengPublic Library of Science (PLoS)PLoS ONE1932-62032015-01-011010e013997910.1371/journal.pone.0139979Microfluidic Leaching of Soil Minerals: Release of K+ from K Feldspar.Davide CiceriAntoine AllanoreThe rate of K+ leaching from soil minerals such as K-feldspar is believed to be too slow to provide agronomic benefit. Currently, theories and methods available to interpret kinetics of mineral processes in soil fail to consider its microfluidic nature. In this study, we measure the leaching rate of K+ ions from a K-feldspar-bearing rock (syenite) in a microfluidic environment, and demonstrate that at the spatial and temporal scales experienced by crop roots, K+ is available at a faster rate than that measured with conventional apparatuses. We present a device to investigate kinetics of mineral leaching at an unprecedented simultaneous resolution of space (~101-102 μm), time (~101-102 min) and fluid volume (~100-101 mL). Results obtained from such a device challenge the notion that silicate minerals cannot be used as alternative fertilizers for tropical soils.http://europepmc.org/articles/PMC4613825?pdf=render
spellingShingle Davide Ciceri
Antoine Allanore
Microfluidic Leaching of Soil Minerals: Release of K+ from K Feldspar.
PLoS ONE
title Microfluidic Leaching of Soil Minerals: Release of K+ from K Feldspar.
title_full Microfluidic Leaching of Soil Minerals: Release of K+ from K Feldspar.
title_fullStr Microfluidic Leaching of Soil Minerals: Release of K+ from K Feldspar.
title_full_unstemmed Microfluidic Leaching of Soil Minerals: Release of K+ from K Feldspar.
title_short Microfluidic Leaching of Soil Minerals: Release of K+ from K Feldspar.
title_sort microfluidic leaching of soil minerals release of k from k feldspar
url http://europepmc.org/articles/PMC4613825?pdf=render
work_keys_str_mv AT davideciceri microfluidicleachingofsoilmineralsreleaseofkfromkfeldspar
AT antoineallanore microfluidicleachingofsoilmineralsreleaseofkfromkfeldspar