O2 distribution and dynamics in the rhizosphere of Phragmites australis, and implications for nutrient removal in sediments
O2 distribution and dynamics in the rhizosphere of Phragmites australis, and implications for nutrient removal in sediments
复制标题
芦苇根际氧气分布和动态及其对沉积物中养分去除的影响
DOI:
10.1016/j.envpol.2021.117193
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发表时间:
2021
影响因子:
8.9
通讯作者:
Yan Wang
中科院分区:
文献类型:
--
作者:
Cai Li;Shiming Ding;Xin Ma;Musong Chen;Zhilin Zhong;Yi Zhang;Mingyi Ren;Min Zhang;Liyuan Yang;Nan Rong;Yan Wang
Root-triggered microscale variations in O2distribution in the rhizosphere of youngPhragmites australisare important for nutrient removal in sediments. In this study, the micro-scale O2dynamics and the small-scale changes of soluble reactive phosphorus (SRP) and ammonium (NH4+) in the rhizosphere ofP. australiswere investigated using planar optodes and high-resolution dialysis (HR-Peeper), respectively. Results suggested that root O2leakage has a highly variable distribution depending on the stage of root growth, the site of O2leakage gradually shift from the entire emerging main roots to the main root tip and subsequently shifted the emerging lateral roots. The O2concentration increased in the rhizosphere with increasing light intensity and O2levels in the overlying water. Continuous O2release from the lateral roots causes the formation of iron plaque on the surface of lateral roots, which reduce the mobility of P by adsorption of iron plaque in the rhizosphere. The oscillation of oxic-anoxic root zones improves nitrogen removal through the processes of anammox, heterotrophic denitrification and nitrification. This work from the micro-scale demonstrates that the O2concentration is the spatio-temporal variations in the rhizosphere, and it presents an important role for nutrient removal in sediments.