STUDY ON THE MECHANISM OF TRANSPORT OF HEAVY METALS IN SOIL IN WESTERN SUBURB OF BEIJING

dc.contributor.authorLi H.
dc.contributor.authorWang J.
dc.contributor.authorTeng Ya.
dc.contributor.authorWang Zh.
dc.date.accessioned2024-10-19T07:54:49Z
dc.date.available2024-10-19T07:54:49Z
dc.date.issued2006
dc.description.abstractResearchers are paying more and more attention to the adsorption and transport of heavy metals in soil. In this study, laboratory experiments were performed to investigate the characteristics of adsorption and transport of mercury in soils of different locations in the western suburb of Beijing. To characterize the adsorption mechanism of mercury in soil, adsorption isotherms were determined through a batch experiment. Soil column experiments were performed in saturated soil under steady-state flow at a specific water head. The breakthrough curves (BTC) for the tracer (bromine) and mercury were obtained after continuous input. Moreover, two solute transport models [convection-dispersion equation model (CDE) and two-site non-equilibrium model (TSN)] were used to simulate heavy metal movement in soil on a laboratory column scale. According to the simulating results, we explored which model is more adapted to simulate the movement of heavy metals in saturated soil in the western suburb of Beijing.
dc.identifierhttps://www.elibrary.ru/item.asp?id=51206978
dc.identifier.citationChinese Journal of Geochemistry, 2006, 25, 2, 173-177
dc.identifier.doi10.1007/bf02872178
dc.identifier.issn1000-9426
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46073
dc.subjectHEAVY METAL
dc.subjectPORE-WATER VELOCITY
dc.subjectRETARDATION FACTOR
dc.subjectTWO-SITE NON-EQUILIBRIUM MODEL
dc.titleSTUDY ON THE MECHANISM OF TRANSPORT OF HEAVY METALS IN SOIL IN WESTERN SUBURB OF BEIJING
dc.typeСтатья

Файлы

Оригинальный пакет

Показано 1 - 1 из 1
Загрузка...
Изображение-миниатюра
Имя:
Li_06.pdf
Размер:
362.7 KB
Формат:
Adobe Portable Document Format

Коллекции