东北林业大学学报
東北林業大學學報
동북임업대학학보
JOURNAL OF NORTHEAST FORESTRY UNIVERSITY
2014年
6期
68-72
,共5页
刘文利%吴景贵%赵新宇%吕岩
劉文利%吳景貴%趙新宇%呂巖
류문리%오경귀%조신우%려암
果园土壤%结合态腐殖质%种植年限%元素组成
果園土壤%結閤態腐殖質%種植年限%元素組成
과완토양%결합태부식질%충식년한%원소조성
Orchard soils%Combined humus%Cultivation years%Elemental composition
以长期冻融条件下的典型中国北方果园土壤为研究对象,分析了不同园龄果园土壤腐殖质的结合态组分数量及其元素组成。结果表明:重组有机碳、松结态、稳结态腐殖质质量分数均逐年增加;紧结态腐殖质质量分数逐年减小。土壤重组有机碳、松结态腐殖质质量分数60 a间分别增加了11.59%、95.15%;果园土壤松/紧比逐年增大,种植60 a年均增长2.09%。近果园荒地土壤腐殖质以紧结态为主,占49.63%,种植60 a时果园土壤腐殖质结合形态以松结态和紧结态为主,分别为41.43%、38.50%;种植果树后,松结态、稳结态比例逐年上升,而紧结态比例逐年下降,松结态腐殖质相对质量分数上升了17.74%,紧结态腐殖质相对质量分数下降了11.13%。果园土壤松结态、稳结态胡敏酸(HA)、富里酸(FA)质量分数及其w(胡敏酸)/w(富里酸)均随种植年限逐年上升。种植果树60 a后,土壤松结态HA、FA质量分数分别增加了131.76%、66.67%。 FA、HA中N、C质量分数逐年上升,H、O质量分数则呈下降趋势;FA、HA中N与C原子数量比均逐年上升且大于近果园荒地;H与C、O与C原子数量比均逐年下降且小于近果园荒地;HA中H与O原子数量比果园土壤均大于近果园荒地。果园土壤稳结态腐殖质HA中的N、C和H元素质量分数均大于FA;HA中O元素质量分数小于FA中O元素质量分数。 FA、HA中N与C、H与O原子数量比均大于近果园荒地土壤,H与C、O与C原子数量比均小于近果园荒地。
以長期凍融條件下的典型中國北方果園土壤為研究對象,分析瞭不同園齡果園土壤腐殖質的結閤態組分數量及其元素組成。結果錶明:重組有機碳、鬆結態、穩結態腐殖質質量分數均逐年增加;緊結態腐殖質質量分數逐年減小。土壤重組有機碳、鬆結態腐殖質質量分數60 a間分彆增加瞭11.59%、95.15%;果園土壤鬆/緊比逐年增大,種植60 a年均增長2.09%。近果園荒地土壤腐殖質以緊結態為主,佔49.63%,種植60 a時果園土壤腐殖質結閤形態以鬆結態和緊結態為主,分彆為41.43%、38.50%;種植果樹後,鬆結態、穩結態比例逐年上升,而緊結態比例逐年下降,鬆結態腐殖質相對質量分數上升瞭17.74%,緊結態腐殖質相對質量分數下降瞭11.13%。果園土壤鬆結態、穩結態鬍敏痠(HA)、富裏痠(FA)質量分數及其w(鬍敏痠)/w(富裏痠)均隨種植年限逐年上升。種植果樹60 a後,土壤鬆結態HA、FA質量分數分彆增加瞭131.76%、66.67%。 FA、HA中N、C質量分數逐年上升,H、O質量分數則呈下降趨勢;FA、HA中N與C原子數量比均逐年上升且大于近果園荒地;H與C、O與C原子數量比均逐年下降且小于近果園荒地;HA中H與O原子數量比果園土壤均大于近果園荒地。果園土壤穩結態腐殖質HA中的N、C和H元素質量分數均大于FA;HA中O元素質量分數小于FA中O元素質量分數。 FA、HA中N與C、H與O原子數量比均大于近果園荒地土壤,H與C、O與C原子數量比均小于近果園荒地。
이장기동융조건하적전형중국북방과완토양위연구대상,분석료불동완령과완토양부식질적결합태조분수량급기원소조성。결과표명:중조유궤탄、송결태、은결태부식질질량분수균축년증가;긴결태부식질질량분수축년감소。토양중조유궤탄、송결태부식질질량분수60 a간분별증가료11.59%、95.15%;과완토양송/긴비축년증대,충식60 a년균증장2.09%。근과완황지토양부식질이긴결태위주,점49.63%,충식60 a시과완토양부식질결합형태이송결태화긴결태위주,분별위41.43%、38.50%;충식과수후,송결태、은결태비례축년상승,이긴결태비례축년하강,송결태부식질상대질량분수상승료17.74%,긴결태부식질상대질량분수하강료11.13%。과완토양송결태、은결태호민산(HA)、부리산(FA)질량분수급기w(호민산)/w(부리산)균수충식년한축년상승。충식과수60 a후,토양송결태HA、FA질량분수분별증가료131.76%、66.67%。 FA、HA중N、C질량분수축년상승,H、O질량분수칙정하강추세;FA、HA중N여C원자수량비균축년상승차대우근과완황지;H여C、O여C원자수량비균축년하강차소우근과완황지;HA중H여O원자수량비과완토양균대우근과완황지。과완토양은결태부식질HA중적N、C화H원소질량분수균대우FA;HA중O원소질량분수소우FA중O원소질량분수。 FA、HA중N여C、H여O원자수량비균대우근과완황지토양,H여C、O여C원자수량비균소우근과완황지。
We analyzed the effect of elemental composition and combined humus of typical orchard soils with different cultivation years in northern China under long-term freezing-thawing conditions.The content of the heavy fraction organic carbon, the loosely combined humus, the stably combined humus are increased with the cultivation year, and the tight combined humus is gradually decreased .The content of the heavy fraction organic carbon and the loosely combined humus annual growth rates are 11.59%and 95.15%in 60 years, respectively.The ratio of loosely and tightly in the orchards soil shows annual increasing trend by 2.09%.On uncultivated area near the orchard, the tight combined humus is main part about 49.63%, the loosely combined humus and the tight combined humus are main parts in the orchards soil, and respectively 11.59%and 95.15%in the 60th year.After the planting of fruit trees, the relative content of the loosely combined humus are in-creased by about 17.74%with the cultivation year, and the relative content of the tight combined humus is gradually de-creased by about 11.13%.The contents of the loosely combined humus acid (HA), the loosely combined fulvic acid (FA) annual growth rates are 131.76% and 66.67% in 60 years, respectively.On elemental composition the loosely combined humus, the contents of nitrogen (N) and carbon(C) are increased with the cultivation year, and hydrogen (H) and oxygen (O) are gradually decreased.N/C is increased and it is higher than that in wasteland soil, and H/C and O/C was opposite.H/O of HA is higher than that in uncultivated area near the orchard.On the stably combined humus in or-chard soil, the contents order of N, C, N is HA>FA, and that of O is HA<FA.N/C is higher than that in wasteland soil, but H/C and O/C are opposite.