4.7 Article

Co-transport of biochar colloids with organic contaminants in soil column

Journal

ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
Volume 28, Issue 2, Pages 1574-1586

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11356-020-10606-5

Keywords

Biochar colloids; Dissolved organic carbon; Organic contaminants; Co-transport; Soil column

Funding

  1. National Key Research and Development Program of China [2017YFA0207003]
  2. National Natural Science Foundation of China [21621005, 21525728]

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This study investigated the co-transport of biochar colloids and organic contaminants in soil, revealing that the enhancement effect of biochar colloids on contaminant transport decreased with increasing charring temperature or particle size of biochar colloids.
Co-transport of biochar (BC) colloids with coexisting organic contaminants (OCs) in soil involves complex interactions among BC colloids, OCs, and soil particles, which is significant for the environmental application and risk assessment of BC and yet has not been well addressed. This study explored co-transports of three typical OCs (i.e., phenanthrene (PHN), atrazine (ATZ), and oxytetracycline (OTC)) and BC colloids obtained from bulk BCs with different charring temperatures (200-700 degrees C) and particle sizes (250 nm, 500 nm, and 1 mu m) in a soil column of 9 cm in height. Considerable transport of BC colloids alone was observed and the maximum breakthrough concentration (C/C-o) increased from 0.08 to 0.77 as the charring temperature decreased from 700 to 200 degrees C. The mobilities of PHN, OTC, and ATZ alone were very low but were greatly increased by co-transports with BC colloids, and their maximumC/C(o)values were within 0.05-0.33, 0.03-0.44, and 0.05-0.62, respectively, in the absence and presence of various BC colloids. The enhancement effect of BC colloids on the OC transport decreased with increasing charring temperature or particle size of BC colloids. BC colloids mainly acted as a vehicle to facilitate the transport of OCs, and dissolved organic carbon from BC colloids also contributed to the increased mobility of OCs in dissolved form. These findings provide new insights into co-transport of BC colloids and contaminants in soil.

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