The Uptake and Accumulation of P Assessed by DGT/Rhizobox Method

Chapter

Abstract

The rhizosphere zone includes the volume of soil or sediment interacting directly and indirectly with the plant roots and the microzone near root with the radial distance from nanometers to centimeters (Hiltner in Arbeiten der Deutschen Landwirtschafts Gesellschafi 98:59–78, 1904). The rhizosphere environment is as complex as the aboveground part of the plant. The rhizosphere is the interface between root and mineral phases, which has the intricate ecological feedback, chemical interaction, and the interorganism communication.

Keywords

Plant Tissue Aquatic Plant Soil Compartment Erhai Lake Linear Regression Curve 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

References

  1. Hiltner L (1904) Uber neuere Erfahrungen und Probleme auf dem Gebiet der Bodenbakteriologie und unter besonderer Beriicksichtigung der Griindiingung und Brache. Arbeiten der Deutschen Landwirtschafts Gesellschafi 98:59–78Google Scholar
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  3. Wu ZH, Wang SR, He MC (2015) Element remobilization, “internal P-loading” and sediment-P reactivity researched by DGT (diffusive gradients in thin films) technique. Environ Sci Pollut R 22:16173–16183CrossRefGoogle Scholar
  4. Youssef RA, Chino M (1988) Development of a new rhizobox system to study the nutrient status in the rhizosphere. Soil Sci Plant Nutr 34:461–465CrossRefGoogle Scholar

Copyright information

© Springer Science+Business Media Singapore 2016

Authors and Affiliations

  1. 1.State Key Laboratory of Environmental Criteria and Risk Assessment, State Environmental Protection Key Laboratory for Lake Pollution ControlResearch Center of Lake Eco-environment, Chinese Research Academy of Environmental SciencesBeijingPeople’s Republic of China

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