4.7 Article

Rhizospheric effects on atrazine speciation and degradation in laterite soils of Pennisetum alopecuroides (L.) Spreng

Journal

ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
Volume 25, Issue 13, Pages 12407-12418

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11356-018-1468-6

Keywords

Pennisetum alopecuroides (L.) Spreng.; Rhizosphere; Atrazine; Diffusive gradients in thin film (DGT); Phytoremediation

Funding

  1. National Natural Science Foundation of China [41301252, 41671235, U1401234]
  2. Natural Science Foundation of Guangdong [2016A030310330, 2017A030310662]
  3. Scientific and Technological Planning Project of Guangzhou, China [201707020034]
  4. Special Fund for Outstanding Young Teachers of Guangdong Ocean University [HDYQ2015007, HDYQ2017004]

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Atrazine (2-chloro-4-ethylamino-6-isopropylamino-1,3,5-triazine) is a worldwide-used herbicide and often detected in agricultural soils and groundwater at concentrations above the permitted limit, because of its high mobility, persistence, and massive application. This study applied pot experiments to investigate the atrazine contents and speciation during the phytoremediation process by Pennisetum alopecuroides (L.) Spreng. in laterite soils. From the change of the total atrazine and bioavailable atrazine measured by diffusive gradients in thin film (DGT), P. alopecuroides significantly improved atrazine degradation efficiency from 15.22 to 51.46%, attributing to the increasing bioavailable atrazine in rhizosphere. Only a small amount of atrazine was taken up by P. alopecuroides root and the acropetal translocation from roots to shoots was limited. The atrazine speciation was significantly different between rhizosphere and non-rhizosphere, attributing to the declining pH and organic matters in rhizosphere. The relationship between pH and soil-bound/humus-fixed atrazine illustrated the pH-dependant release of the atrazine from soils and the competition between humus adsorption and uptake by P. alopecuroides. The present study reveals the important roles of soil pH and organic matters in atrazine speciation and availability in laterite soils, and provides new insights in the rhizospheric effects on effective phytoremediation of atrazine.

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