农业环境科学学报
農業環境科學學報
농업배경과학학보
Journal of Agro-Environment Science
2014年
4期
687-694
,共8页
柳勇%于雄胜%李芳柏%徐建明%楼骏%刘传平
柳勇%于雄勝%李芳柏%徐建明%樓駿%劉傳平
류용%우웅성%리방백%서건명%루준%류전평
紫云英%水溶性有机物%潜育水耕人为土%五氯酚%活性铁形态%连续提取%逐步回归模型
紫雲英%水溶性有機物%潛育水耕人為土%五氯酚%活性鐵形態%連續提取%逐步迴歸模型
자운영%수용성유궤물%잠육수경인위토%오록분%활성철형태%련속제취%축보회귀모형
Chinese milk vetch%dissolved organic matter%Gleyi-Stagnic Anthrosol%pentachlorophenol%active iron species%sequential extrac-tion%stepwise regression model
以潜育水耕人为土为供试土壤,以不同的处理方式和培养时间下产生的紫云英水溶性有机物(DOM)为添加物(包括新鲜紫云英 DOM、淹水腐解7 d 和14 d 紫云英 DOM、好气腐解7 d 和14 d 紫云英 DOM;800 mg C·L-1),研究了5种 DOM 作为有机碳源促进淹水土壤中五氯酚(PCP)还原转化与 Fe(Ⅱ)累积的关系。结果表明,紫云英 DOM 在淹水6.5 d 后均可显著促进 PCP 的还原(P﹤0.05),淹水2 d 后显著促进了乙酸钠提取态 Fe(Ⅱ)[Fe(Ⅱ)NaOAc]和乙酸钠﹢盐酸连续提取态 Fe(Ⅱ)[Fe(Ⅱ)NaOAc﹢HCl]的累积(P﹤0.05);多数情况下还可促进乙酸钠提取态 Fe(Ⅲ)[Fe(Ⅲ)NaOAc]的累积;多元线性回归分析发现,PCP 还原主要受 Fe(Ⅱ)NaOAc﹢HCl 影响,其逐步回归模型为:PCP(mg·kg-1)=22.95-0.047Fe(Ⅱ)NaOAc﹢HCl(mg·kg-1)(R2=0.615,P﹤0.01)。因此,DOM 促进了淹水土壤中 PCP 还原与铁还原,Fe(Ⅱ)累积是导致 PCP 还原转化的主要化学机制。
以潛育水耕人為土為供試土壤,以不同的處理方式和培養時間下產生的紫雲英水溶性有機物(DOM)為添加物(包括新鮮紫雲英 DOM、淹水腐解7 d 和14 d 紫雲英 DOM、好氣腐解7 d 和14 d 紫雲英 DOM;800 mg C·L-1),研究瞭5種 DOM 作為有機碳源促進淹水土壤中五氯酚(PCP)還原轉化與 Fe(Ⅱ)纍積的關繫。結果錶明,紫雲英 DOM 在淹水6.5 d 後均可顯著促進 PCP 的還原(P﹤0.05),淹水2 d 後顯著促進瞭乙痠鈉提取態 Fe(Ⅱ)[Fe(Ⅱ)NaOAc]和乙痠鈉﹢鹽痠連續提取態 Fe(Ⅱ)[Fe(Ⅱ)NaOAc﹢HCl]的纍積(P﹤0.05);多數情況下還可促進乙痠鈉提取態 Fe(Ⅲ)[Fe(Ⅲ)NaOAc]的纍積;多元線性迴歸分析髮現,PCP 還原主要受 Fe(Ⅱ)NaOAc﹢HCl 影響,其逐步迴歸模型為:PCP(mg·kg-1)=22.95-0.047Fe(Ⅱ)NaOAc﹢HCl(mg·kg-1)(R2=0.615,P﹤0.01)。因此,DOM 促進瞭淹水土壤中 PCP 還原與鐵還原,Fe(Ⅱ)纍積是導緻 PCP 還原轉化的主要化學機製。
이잠육수경인위토위공시토양,이불동적처리방식화배양시간하산생적자운영수용성유궤물(DOM)위첨가물(포괄신선자운영 DOM、엄수부해7 d 화14 d 자운영 DOM、호기부해7 d 화14 d 자운영 DOM;800 mg C·L-1),연구료5충 DOM 작위유궤탄원촉진엄수토양중오록분(PCP)환원전화여 Fe(Ⅱ)루적적관계。결과표명,자운영 DOM 재엄수6.5 d 후균가현저촉진 PCP 적환원(P﹤0.05),엄수2 d 후현저촉진료을산납제취태 Fe(Ⅱ)[Fe(Ⅱ)NaOAc]화을산납﹢염산련속제취태 Fe(Ⅱ)[Fe(Ⅱ)NaOAc﹢HCl]적루적(P﹤0.05);다수정황하환가촉진을산납제취태 Fe(Ⅲ)[Fe(Ⅲ)NaOAc]적루적;다원선성회귀분석발현,PCP 환원주요수 Fe(Ⅱ)NaOAc﹢HCl 영향,기축보회귀모형위:PCP(mg·kg-1)=22.95-0.047Fe(Ⅱ)NaOAc﹢HCl(mg·kg-1)(R2=0.615,P﹤0.01)。인차,DOM 촉진료엄수토양중 PCP 환원여철환원,Fe(Ⅱ)루적시도치 PCP 환원전화적주요화학궤제。
This study investigated the effects of dissolved organic matter(DOM)from green manure on pentachlorophenol(PCP)reduc-tive transformation and Fe(Ⅲ)reduction under flooded soil conditions. Batch experiments were conducted to explore the kinetics of PCP reductive transformation and its relationship with Fe(Ⅱ)accumulation in a flooded paddy soil(Gleyi-Stagnic Anthrosol)amended with fresh or decomposed(continuously-flooded, CF or non-flooded, NF; 7 and 14 d)DOM from Chinese milk vetch(Astragalus sinicus L., CMV; 800 mg C·L-1). The 5 treatments of CMV-derived DOM(CMV-DOM)significantly enhanced the reductive transformation of PCP and the accumulation of NaOAc-extractable or sequential NaOAc- and HCl-extractable Fe(Ⅱ)[Fe(Ⅱ)NaOAc﹢HCl] after 6.5 and 2 d of flooding, respectively(P﹤0.05). In most cases, the addition of CMV-DOM greatly increased NaOAc-extractable Fe(Ⅲ)owing to non-reductive dissolution. The relationship between reduction kinetics and selected environmental variables was examined by correlation analysis and regression analysis . Sequential NaOAc-and HCl-extractable Fe(Ⅱ)was found playing a vital role in PCP reductive transformation, and a stepwise regression model was established as follows: PCP(mg·kg-1)=22.95-0.047Fe(Ⅱ)NaOAc﹢HCl(mg·kg -1)(R2=0.615, P﹤0.01). The results demonstrated that addition of CMV-DOM accelerated PCP reductive transformation and Fe(Ⅲ)reduction in the flooded paddy soil. In terms of soil chemistry, enhanced PCP reductive transformation in flooded paddy soil is attributable to gen-eration of adsorbed Fe(Ⅱ)with high redox activity.