应用生态学报
應用生態學報
응용생태학보
CHINESE JOURNAL OF APPLIED ECOLOGY
2001年
2期
233-236
,共4页
Mn有效性%硝酸盐%土壤水分%湿-干循环
Mn有效性%硝痠鹽%土壤水分%濕-榦循環
Mn유효성%초산염%토양수분%습-간순배
在[Ca(NO3)2]盐处理土壤中,研究了两种湿度水平(200、400g·kg-1)和湿-干循环对土壤Mn释放的影响.结果表明,土壤水分状况影响土壤Mn的有效性,湿度大时,易还原态Mn转化为水溶态、交换态Mn;盐分对易还原态Mn的转化有一定影响,NO3-能缓冲土壤Eh的下降,有抑制易还原态Mn转化的作用.连续的湿-干循环能使土壤2价Mn(水溶态Mn、交换态Mn)浓度降低,而Ca(NO3)2盐能增加Mn的不溶性.这在Mn含量低的土壤上,最终将导致Mn的缺乏.
在[Ca(NO3)2]鹽處理土壤中,研究瞭兩種濕度水平(200、400g·kg-1)和濕-榦循環對土壤Mn釋放的影響.結果錶明,土壤水分狀況影響土壤Mn的有效性,濕度大時,易還原態Mn轉化為水溶態、交換態Mn;鹽分對易還原態Mn的轉化有一定影響,NO3-能緩遲土壤Eh的下降,有抑製易還原態Mn轉化的作用.連續的濕-榦循環能使土壤2價Mn(水溶態Mn、交換態Mn)濃度降低,而Ca(NO3)2鹽能增加Mn的不溶性.這在Mn含量低的土壤上,最終將導緻Mn的缺乏.
재[Ca(NO3)2]염처리토양중,연구료량충습도수평(200、400g·kg-1)화습-간순배대토양Mn석방적영향.결과표명,토양수분상황영향토양Mn적유효성,습도대시,역환원태Mn전화위수용태、교환태Mn;염분대역환원태Mn적전화유일정영향,NO3-능완충토양Eh적하강,유억제역환원태Mn전화적작용.련속적습-간순배능사토양2개Mn(수용태Mn、교환태Mn)농도강저,이Ca(NO3)2염능증가Mn적불용성.저재Mn함량저적토양상,최종장도치Mn적결핍.
A study on the effects of two moisture levels (200 and 400g.kg-1) and wetting-drying on the solubility of Mn in Ca
(NO3)2-amended soils showed that water regime was a factor affecting Mn availability. Easily reducible Mn was trans
formed into soluble and exchangeable Mn, when soil water content was high. Salt had a definite effect on the transfor
mation of easily reducible Mn. NO3- could decrease soil redox potential, and inhibit the transformation of easily re
ducible Mn. Wetting-drying significantly(a< 0.05) decreased the content of soil water-soluble and exchangeable Mn,
while Ca(NO3)2 increased the insolubility of Mn, which might eventually lead to the deficiency of soil Mn.