新疆大学学报(自然科学版)
新疆大學學報(自然科學版)
신강대학학보(자연과학판)
XINJIANG UNIVERSITY JOURNAL(NATURAL SCIENCE EDITION)
2013年
3期
257-261
,共5页
土壤养分%水盐%通径分析%克里雅河流域
土壤養分%水鹽%通徑分析%剋裏雅河流域
토양양분%수염%통경분석%극리아하류역
soil nutrients%water-salt properties%path analysis%Keriya River watershed
选择克里雅河流域于田绿洲为研究区,以绿洲土、盐渍土、棕漠土及风沙土等4种类型土壤为对象,分析了土壤表层养分、水盐因子的特征,结合通径分析方法研究了养分与水盐的相关关系。结果表明:不同土壤类型土壤养分与水盐因子差异性显著。通径分析显示,土壤水分对有机质含量和全氮的直接作用显著,地下水埋深通过土壤水对有机质和全氮的间接通径系数较大;水盐因子可能不是影响有效磷的主要因素;虽然水分因子对速效钾的直接通径系数较大,但其综合影响较校?盐分因子对速效钾的影响较大。
選擇剋裏雅河流域于田綠洲為研究區,以綠洲土、鹽漬土、棕漠土及風沙土等4種類型土壤為對象,分析瞭土壤錶層養分、水鹽因子的特徵,結閤通徑分析方法研究瞭養分與水鹽的相關關繫。結果錶明:不同土壤類型土壤養分與水鹽因子差異性顯著。通徑分析顯示,土壤水分對有機質含量和全氮的直接作用顯著,地下水埋深通過土壤水對有機質和全氮的間接通徑繫數較大;水鹽因子可能不是影響有效燐的主要因素;雖然水分因子對速效鉀的直接通徑繫數較大,但其綜閤影響較校?鹽分因子對速效鉀的影響較大。
선택극리아하류역우전록주위연구구,이록주토、염지토、종막토급풍사토등4충류형토양위대상,분석료토양표층양분、수염인자적특정,결합통경분석방법연구료양분여수염적상관관계。결과표명:불동토양류형토양양분여수염인자차이성현저。통경분석현시,토양수분대유궤질함량화전담적직접작용현저,지하수매심통과토양수대유궤질화전담적간접통경계수교대;수염인자가능불시영향유효린적주요인소;수연수분인자대속효갑적직접통경계수교대,단기종합영향교교?염분인자대속효갑적영향교대。
Soil samples from 0-20 cm layers under different soil types (oasis soil, brown desert soil, saline soil and aeolian sandy soil) were collected across Yutian oasis of the Keriya river watershed. By analyzing soil nutrients and water-salt properties, this study made an attempt to discuss the relationships between soil nutrients and water-salt properties by the methods of path analysis. The results showed that there were differences among different soil types in terms of soil nutrients and water-salt properties. Path analysis showed that soil moisture had a significant relationship with soil organic matter and total nitrogen while groundwater depth was indirectly related to soil organic matter and total nitrogen. Water-salt properties were not the important factors affecting available P. The available K was determined largely by salt factors though the direct path coefficients to water properties were bigger.