摘要
磷危机"与"水体富营养化"现象随行,致污水磷回收势在必行。最近,在污泥厌氧消化过程中发现了磷回收新产物——蓝铁矿,一种化学稳定性很强、回收用途极为广泛、经济价值更高的磷酸盐化合物。鉴于此,通过试验验证污泥厌氧消化条件下,Fe~(3+)生物还原至Fe~(2+)、与污泥释放的PO_4~(3-)反应生成蓝铁矿的可行性以及所需环境条件与限制因素。结果显示,Fe~(3+)在厌氧消化过程中会被异化金属还原菌(DMRB)还原为Fe~(2+),与污泥细胞裂解释放出的PO_4~(3-)可以生成蓝铁矿,含量高达204 mg/g DS。进言之,碳酸盐(MCO_3)不会干扰蓝铁矿生成。Fe~(3+)被生物还原时,DMRB会与产甲烷菌(MPB)争夺电子供体(有机物),一方面会抑制厌氧消化产甲烷(CH_4),另一方面,Fe~(3+)也提供了MPB所必需的Fe元素,可刺激酶活,反而能促进产CH_4过程;Fe~(3+)对产CH_4过程的综合影响为促进作用。
Phosphorus crisis"occurs along with"eutrophication"simultaneously,which results in essential P-recovery.Recently,a new product of P-recovery,Fe_3(PO_4)_2·8H_2O(vivianite),was observed in anaerobic digestion(AD)of excess sludge,which is a phosphate compound with a better chemical stability,more extensive applications and higher economic values.For this reason,experiments were conducted to verify the biological reduction of Fe~(3+)into Fe~(2+),to observe the chemical formation of Fe~(2+)with PO_4~(3-)released from sludge under AD and to ascertain environmental conditions and limited factors.The experimental results indicated that Fe~(3+)was biologically reduced into Fe~(2+)by dissimilation metal reducing bacteria(DMRB)under AD,with which PO_4~(3-)released from sludge was combined to form vivianite,up to 204 mg/g DS.Furthermore,carbonate(MCO_3)in the AD system did not interfere with the formation of vivianite.When Fe~(3+)was biologically reduced,DMRB competed with methane production bacteria(MPB)for electron donors(organics),which could inhibit methane(CH_4)production and could on the other hand promote CH_4 production; the comprehensive effect of Fe~(3+) on CH_4 production was positive.
引文
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