Si and Water Management Drives Changes in Fe and Mn Pools that Affect As Cycling and Uptake in Rice

Arsenic availability to rice is tied to biogeochemical cycling of Fe and Mn in rice soils. Two strategies to minimize As uptake by rice—increasing Si and decreasing water—affect soil Fe and Mn pools. We synthesized data from several soil-based experiments with four rice cultivars...

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Main Authors: Angelia L. Seyfferth, Matt Limmer, Weida Wu
Format: Article
Language:English
Published: MDPI AG 2019-08-01
Series:Soil Systems
Subjects:
Online Access:https://www.mdpi.com/2571-8789/3/3/58
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author Angelia L. Seyfferth
Matt Limmer
Weida Wu
author_facet Angelia L. Seyfferth
Matt Limmer
Weida Wu
author_sort Angelia L. Seyfferth
collection DOAJ
description Arsenic availability to rice is tied to biogeochemical cycling of Fe and Mn in rice soils. Two strategies to minimize As uptake by rice—increasing Si and decreasing water—affect soil Fe and Mn pools. We synthesized data from several soil-based experiments with four rice cultivars across pot and field trials with manipulations of Si, water, or both. Increasing Si alters the mineral composition of Fe plaque more than decreasing water, with the former promoting relatively more ferrihydrite and less lepidocrocite. Nonflooded conditions decrease lepidocrocite but slightly increase goethite compared to flooded rice. Plaque As, which was a mixture of arsenite (15−40%) and arsenate (60−85%), was correlated positively with ferrihydrite and negatively with lepidocrocite and goethite. Plaque As was also positively correlated with F1 and F2 soil As, and F2 was correlated positively with porewater As, total grain As, and grain organic As (oAs). Grain inorganic As (iAs) was negatively correlated with oxalate-extractable Fe and Mn. Our data and multiple linear regression models suggest that under flooded conditions iAs is released by poorly crystalline Fe oxides to porewater mainly as iAs(III), which can either be taken up by the plant, adsorbed to Fe plaque, oxidized to iAs(V) or methylated to oAs. Increasing Si can promote more desorption of iAs(III) and promote more poorly-ordered phases in plaque and in bulk soil. The ultimate effectiveness of a Si amendment to decrease As uptake by rice depends upon it being able to increase exogenous Si relative to As in porewater after competitive adsorption/desorption processes. Our data further suggest that poorly crystalline Fe and Mn soil pools can retain inorganic As and decrease plant uptake, but these pools in bulk soil and plaque control grain organic As.
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spelling doaj.art-d45a737083d04a1a8f147b79dd8506652022-12-22T03:07:50ZengMDPI AGSoil Systems2571-87892019-08-01335810.3390/soilsystems3030058soilsystems3030058Si and Water Management Drives Changes in Fe and Mn Pools that Affect As Cycling and Uptake in RiceAngelia L. Seyfferth0Matt Limmer1Weida Wu2Department of Plant and Soil Sciences, University of Delaware, Newark, DE 19716, USADepartment of Plant and Soil Sciences, University of Delaware, Newark, DE 19716, USADepartment of Plant and Soil Sciences, University of Delaware, Newark, DE 19716, USAArsenic availability to rice is tied to biogeochemical cycling of Fe and Mn in rice soils. Two strategies to minimize As uptake by rice—increasing Si and decreasing water—affect soil Fe and Mn pools. We synthesized data from several soil-based experiments with four rice cultivars across pot and field trials with manipulations of Si, water, or both. Increasing Si alters the mineral composition of Fe plaque more than decreasing water, with the former promoting relatively more ferrihydrite and less lepidocrocite. Nonflooded conditions decrease lepidocrocite but slightly increase goethite compared to flooded rice. Plaque As, which was a mixture of arsenite (15−40%) and arsenate (60−85%), was correlated positively with ferrihydrite and negatively with lepidocrocite and goethite. Plaque As was also positively correlated with F1 and F2 soil As, and F2 was correlated positively with porewater As, total grain As, and grain organic As (oAs). Grain inorganic As (iAs) was negatively correlated with oxalate-extractable Fe and Mn. Our data and multiple linear regression models suggest that under flooded conditions iAs is released by poorly crystalline Fe oxides to porewater mainly as iAs(III), which can either be taken up by the plant, adsorbed to Fe plaque, oxidized to iAs(V) or methylated to oAs. Increasing Si can promote more desorption of iAs(III) and promote more poorly-ordered phases in plaque and in bulk soil. The ultimate effectiveness of a Si amendment to decrease As uptake by rice depends upon it being able to increase exogenous Si relative to As in porewater after competitive adsorption/desorption processes. Our data further suggest that poorly crystalline Fe and Mn soil pools can retain inorganic As and decrease plant uptake, but these pools in bulk soil and plaque control grain organic As.https://www.mdpi.com/2571-8789/3/3/58riceFe plaquearsenicsiliconwater management
spellingShingle Angelia L. Seyfferth
Matt Limmer
Weida Wu
Si and Water Management Drives Changes in Fe and Mn Pools that Affect As Cycling and Uptake in Rice
Soil Systems
rice
Fe plaque
arsenic
silicon
water management
title Si and Water Management Drives Changes in Fe and Mn Pools that Affect As Cycling and Uptake in Rice
title_full Si and Water Management Drives Changes in Fe and Mn Pools that Affect As Cycling and Uptake in Rice
title_fullStr Si and Water Management Drives Changes in Fe and Mn Pools that Affect As Cycling and Uptake in Rice
title_full_unstemmed Si and Water Management Drives Changes in Fe and Mn Pools that Affect As Cycling and Uptake in Rice
title_short Si and Water Management Drives Changes in Fe and Mn Pools that Affect As Cycling and Uptake in Rice
title_sort si and water management drives changes in fe and mn pools that affect as cycling and uptake in rice
topic rice
Fe plaque
arsenic
silicon
water management
url https://www.mdpi.com/2571-8789/3/3/58
work_keys_str_mv AT angelialseyfferth siandwatermanagementdriveschangesinfeandmnpoolsthataffectascyclinganduptakeinrice
AT mattlimmer siandwatermanagementdriveschangesinfeandmnpoolsthataffectascyclinganduptakeinrice
AT weidawu siandwatermanagementdriveschangesinfeandmnpoolsthataffectascyclinganduptakeinrice