Plant Functions in Wetland and Aquatic Systems: Influence of Intensity and Capacity of Soil Reduction

Wetland or hydric soils, in addition to excess water and limited air-filled porosity, are characterized by anaerobic or reducing conditions. Wetland plants have developed physiological and morphological adaptations for growing under these conditions. Various methods exist for measuring plant respons...

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Main Authors: R.D. DeLaune, S.R. Pezeshki
Format: Article
Language:English
Published: Wiley 2001-01-01
Series:The Scientific World Journal
Online Access:http://dx.doi.org/10.1100/tsw.2001.257
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author R.D. DeLaune
S.R. Pezeshki
author_facet R.D. DeLaune
S.R. Pezeshki
author_sort R.D. DeLaune
collection DOAJ
description Wetland or hydric soils, in addition to excess water and limited air-filled porosity, are characterized by anaerobic or reducing conditions. Wetland plants have developed physiological and morphological adaptations for growing under these conditions. Various methods exist for measuring plant responses to reducing conditions in wetland and aquatic environments, including assessment of radial oxygen transport, cellular enzymatic transformations, changes in root structure, and nutrient uptake. However, a gap exists in quantifying the chemical properties and reducing nature of soil environment in which plant roots are grown. The variation in reducing conditions, oxygen demand, and other associated processes that occur in wetland soils makes it difficult to truly compare the plant responses reported in the literature. This review emphasizes soil-plant interactions in wetlands, drawing attention to the importance of quantifying the intensity and capacity of reduction and/or oxygen demand in wetland soils to allow proper evaluation of wetland plant responses to such conditions.
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spelling doaj-art-f4911e8c566349e68555c0eb074993132025-02-03T01:24:16ZengWileyThe Scientific World Journal1537-744X2001-01-01163664910.1100/tsw.2001.257Plant Functions in Wetland and Aquatic Systems: Influence of Intensity and Capacity of Soil ReductionR.D. DeLaune0S.R. Pezeshki1Louisiana State University, Wetland Biogeochemistry Institute, Baton Rouge, LA 70803, USALouisiana State University, Wetland Biogeochemistry Institute, Baton Rouge, LA 70803, USAWetland or hydric soils, in addition to excess water and limited air-filled porosity, are characterized by anaerobic or reducing conditions. Wetland plants have developed physiological and morphological adaptations for growing under these conditions. Various methods exist for measuring plant responses to reducing conditions in wetland and aquatic environments, including assessment of radial oxygen transport, cellular enzymatic transformations, changes in root structure, and nutrient uptake. However, a gap exists in quantifying the chemical properties and reducing nature of soil environment in which plant roots are grown. The variation in reducing conditions, oxygen demand, and other associated processes that occur in wetland soils makes it difficult to truly compare the plant responses reported in the literature. This review emphasizes soil-plant interactions in wetlands, drawing attention to the importance of quantifying the intensity and capacity of reduction and/or oxygen demand in wetland soils to allow proper evaluation of wetland plant responses to such conditions.http://dx.doi.org/10.1100/tsw.2001.257
spellingShingle R.D. DeLaune
S.R. Pezeshki
Plant Functions in Wetland and Aquatic Systems: Influence of Intensity and Capacity of Soil Reduction
The Scientific World Journal
title Plant Functions in Wetland and Aquatic Systems: Influence of Intensity and Capacity of Soil Reduction
title_full Plant Functions in Wetland and Aquatic Systems: Influence of Intensity and Capacity of Soil Reduction
title_fullStr Plant Functions in Wetland and Aquatic Systems: Influence of Intensity and Capacity of Soil Reduction
title_full_unstemmed Plant Functions in Wetland and Aquatic Systems: Influence of Intensity and Capacity of Soil Reduction
title_short Plant Functions in Wetland and Aquatic Systems: Influence of Intensity and Capacity of Soil Reduction
title_sort plant functions in wetland and aquatic systems influence of intensity and capacity of soil reduction
url http://dx.doi.org/10.1100/tsw.2001.257
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