Huang Guoxin, Liu Fei, Yang Yingzhao, Kong Xiangke, Li Shengpin, Zhang Ying, Cao Dejun
Beijing Key Laboratory of Water Resources & Environmental Engineering, China University of Geosciences, Beijing, Beijing, 100083, China.
Environ Sci Pollut Res Int. 2015 Mar;22(5):3705-14. doi: 10.1007/s11356-014-3602-4. Epub 2014 Sep 27.
A novel sequential permeable reactive barrier (multibarrier), composed of oxygen-releasing compound (ORC)/clinoptilolite/spongy iron zones in series, was proposed for ammonium-nitrogen-contaminated groundwater remediation. Column experiments were performed to: (1) evaluate the overall NH4(+)-N removal performance of the proposed multibarrier, (2) investigate nitrogen transformation in the three zones, (3) determine the reaction front progress, and (4) explore cleanup mechanisms for inorganic nitrogens. The results showed that NH4 (+)-N percent removal by the multibarrier increased up to 90.43 % after 21 pore volumes (PVs) at the influent dissolved oxygen of 0.68∼2.45 mg/L and pH of 6.76∼7.42. NH4(+)-N of 4.06∼10.49 mg/L was depleted and NOx(-)-N (i.e., NO3 (-)-N + NO2(-)-N) of 4.26∼9.63 mg/L was formed before 98 PVs in the ORC zone. NH4(+)-N of ≤4.76 mg/L was eliminated in the clinoptilolite zone. NOx(-)-N of 10.44∼12.80 mg/L was lost before 21 PVs in the spongy iron zone. The clinoptilolite zone length should be reduced to 30 cm. Microbial nitrification played a dominant role in NH4(+)-N removal in the ORC zone. Ion exchange was majorly responsible for NH4(+)-N elimination in the clinoptilolite zone. Chemical reduction and hydrogenotrophic denitrification both contributed to NOx(-)-N transformation, but the chemical reduction capacity decreased after 21 PVs in the spongy iron.
提出了一种新型的串联式可渗透反应屏障(多屏障),其由释氧化合物(ORC)/斜发沸石/海绵铁区域串联组成,用于修复受铵氮污染的地下水。进行了柱实验以:(1)评估所提出的多屏障对NH4(+)-N的整体去除性能,(2)研究三个区域中的氮转化,(3)确定反应前沿的进展,以及(4)探索无机氮污染物的清除机制。结果表明,在进水溶解氧为0.68∼2.45 mg/L、pH为6.76∼7.42的条件下,经过21个孔隙体积(PVs)后,多屏障对NH4(+)-N的去除率提高到了90.43%。在ORC区域中,在98个PVs之前,4.06∼10.49 mg/L的NH4(+)-N被消耗,同时形成了4.26∼9.63 mg/L的NOx(-)-N(即NO3 (-)-N + NO2(-)-N)。在斜发沸石区域中,≤4.76 mg/L的NH4(+)-N被去除。在海绵铁区域中,在21个PVs之前,10.44∼12.80 mg/L 的NOx(-)-N被去除。斜发沸石区域的长度应减少到30 cm。微生物硝化作用在ORC区域中对NH4(+)-N的去除起主导作用。离子交换是斜发沸石区域中NH4(+)-N去除的主要原因。化学还原和氢营养型反硝化作用都对NOx(-)-N的转化有贡献,但在海绵铁区域中,经过21个PVs后,化学还原能力下降。