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- W156941902 abstract "Wetland plant rhizospheres are often aerobic and oxidized, while bulk soil is anaerobic and chemically reduced. As a result, metals tend to be immobile in the bulk soil but are mobilized by plant-induced changes in the rhizosphere. This leads to enrichment of metals near the roots and enhanced availability for uptake by plants. The apparent metal tolerance of wetland plants compared to dryland plants, without the development of separate metal-tolerant ecotypes, is because of the relatively high exposure of plant roots to metals under the soil conditions prevailing in wetlands. To live in the anaerobic soil conditions, wetland plants have developed root morphology different from that of dryland plants. Many species have porous roots for the supply of oxygen for root respiration, often forming a specialized tissue known as aerenchyma or air tissue. This supply of oxygen is thought to be more than sufficient for root respiration, and excess oxygen may leak into the rhizosphere." @default.
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- W156941902 date "2004-01-01" @default.
- W156941902 modified "2023-10-17" @default.
- W156941902 title "Biogeochemistry of Metals in the Rhizosphere of Wetland Plants — An Explanation for “Innate” Metal Tolerance?" @default.
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- W156941902 doi "https://doi.org/10.1016/b978-044451691-6/50009-0" @default.
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