土壤
土壤
토양
SOILS
2009年
5期
726-732
,共7页
董国涛%张爱娟%罗格平%许文强%戴丽
董國濤%張愛娟%囉格平%許文彊%戴麗
동국도%장애연%라격평%허문강%대려
干旱区绿洲%微量元素%有效性
榦旱區綠洲%微量元素%有效性
간한구록주%미량원소%유효성
Arid area oasis%Trace elements%Availability
土壤微量元素的含量与分布特征是反映特定地区环境状况的一个重要因素,对土地资源的合理开发和利用具有重要意义.本研究以天山北坡三工河流域冲积平原型绿洲为研究区,选择盐土、潮土和灰漠土3种土壤类型,分析其B、Mn、Zn、Fe、Cu等微量元素的有效含量特征.结果表明:⑴以"全国农业系统的土壤速效微量元素丰缺指标"为标准,土壤有效Mn含量属于极低水平,有效Zn和Fe含量属于中等水平,有效Cu属于丰富水平,有效B属于极富水平;⑵三工河流域绿洲土壤中有效Mn、Zn、Fe、Cu含量与土壤pH呈负相关关系;土壤有机质对有效Fe、Cu含量影响很大;有机质和Mn的关系不明显,这和湿润地区研究结果存在显著差异;⑶不同的土壤类型对于土壤有效B、Zn和Fe的含量影响显著;潮土中微量元素的有效含量与盐土、灰漠土中含量相比有显著差异.
土壤微量元素的含量與分佈特徵是反映特定地區環境狀況的一箇重要因素,對土地資源的閤理開髮和利用具有重要意義.本研究以天山北坡三工河流域遲積平原型綠洲為研究區,選擇鹽土、潮土和灰漠土3種土壤類型,分析其B、Mn、Zn、Fe、Cu等微量元素的有效含量特徵.結果錶明:⑴以"全國農業繫統的土壤速效微量元素豐缺指標"為標準,土壤有效Mn含量屬于極低水平,有效Zn和Fe含量屬于中等水平,有效Cu屬于豐富水平,有效B屬于極富水平;⑵三工河流域綠洲土壤中有效Mn、Zn、Fe、Cu含量與土壤pH呈負相關關繫;土壤有機質對有效Fe、Cu含量影響很大;有機質和Mn的關繫不明顯,這和濕潤地區研究結果存在顯著差異;⑶不同的土壤類型對于土壤有效B、Zn和Fe的含量影響顯著;潮土中微量元素的有效含量與鹽土、灰漠土中含量相比有顯著差異.
토양미량원소적함량여분포특정시반영특정지구배경상황적일개중요인소,대토지자원적합리개발화이용구유중요의의.본연구이천산북파삼공하류역충적평원형록주위연구구,선택염토、조토화회막토3충토양류형,분석기B、Mn、Zn、Fe、Cu등미량원소적유효함량특정.결과표명:⑴이"전국농업계통적토양속효미량원소봉결지표"위표준,토양유효Mn함량속우겁저수평,유효Zn화Fe함량속우중등수평,유효Cu속우봉부수평,유효B속우겁부수평;⑵삼공하류역록주토양중유효Mn、Zn、Fe、Cu함량여토양pH정부상관관계;토양유궤질대유효Fe、Cu함량영향흔대;유궤질화Mn적관계불명현,저화습윤지구연구결과존재현저차이;⑶불동적토양류형대우토양유효B、Zn화Fe적함량영향현저;조토중미량원소적유효함량여염토、회막토중함량상비유현저차이.
Taking the alluvial plain oasis as a study case, the available contents of B, Mn, Zn, Fe, and Cu in three soil types were analyzed with SPSS. The results showed that:①According to "Plentiful-lack index of soil available trace elements in Agricultural Libraries all over China", available Mn was insufficient, available Zn and Fe were moderate, available Cu was rich, and available B was very plentiful.②Significant negative correlations were observed between available contents of Mn, Zn, Fe, Cu and soil pH. The effect of organic matter content on available Fe and Cu was significant in arid area oasis, which was significantly different from humid area.③There were differences in available contents of B, Zn and Fe among different soil types, the available contents of trace elements in the alluvial soil were significantly different from the saline soil and gray desert soil.