白云石
估价
生物炭
环境科学
修正案
石灰
土壤改良剂
蚯蚓粪
土壤水分
农学
壤土
环境化学
环境工程
环境修复
生物量(生态学)
砷
化学
植被恢复
污染物
稻草
土壤污染
土壤管理
营养物
植被(病理学)
温室
土壤pH值
锌
地表径流
浸出(土壤学)
土壤肥力
土壤分类
温室气体
土壤质量
作者
Lorena Salgado,J.R. Gallego,Roberto Caballero,María Larramona,Elías Afif Khouri,Maximino Herías,Raquel Lara,Juan M. Menéndez-Aguado,Rubén Forján
标识
DOI:10.1016/j.jenvman.2025.127795
摘要
/kg), and reduced Al saturation (11.2 % → ∼0.02 %), with large decreases in TCLP-Cu fell to <10 mg/kg in dolomite-containing treatments and to <3 mg/kg with VC formulations; Zn was suppressed to <65 mg/kg except where liming counteracted B effects. Arsenic showed a distinct pattern: VC increased TCLP-As in close association with available P, whereas dolomite alone or with B kept As below detection-most plausibly via Ca/Mg-driven (co)precipitation of sparingly soluble arsenate/phosphate phases; notably, SVD < SV for As, indicating partial mitigation by dolomite. Vegetation failed in the control but established across all amended soils, with biomass maximized under VC. Overall, the results indicate that dolomite by-product particularly in combination with VC provides a circular, field-relevant route to restore soil function and reduce bioavailable Cu and Zn by >90 % while sustaining plant establishment; given VC-linked As mobilization, co-amendment with Fe-rich sorbents and prudent P management are recommended to minimize risk in practical applications.
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