首页|川黄檗不同树龄矿质元素含量及其与根际土壤因子的相关性分析

川黄檗不同树龄矿质元素含量及其与根际土壤因子的相关性分析

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[目的]探究川黄檗不同树龄各部位和根际土壤中矿质元素含量变化规律,以及矿质元素和土壤因子相关性,以期为川黄檗幼龄林营养诊断、科学施肥提供依据。[方法]以川黄檗 1~3 年生苗木为试材,对不同部位(叶、当年生枝和根)和根际土壤中矿质元素含量及其变化规律进行研究,并分析了根际土壤与不同部位间以及各部位中矿质元素间的相关性,进而评价不同部位对土壤中矿质营养元素的富集能力。[结果]1)不同树龄和不同部位矿质元素含量具有一定的差异,且随着树龄的增加,叶中N、Ca、Cu和Zn,当年生枝中P和Cu以及根中Mg含量显著下降(P<0。05)。2)不同树龄根际土壤矿质元素含量差异显著(P<0。05),随着树龄增加,Ca、Mn和Zn含量显著增加(P<0。05),Fe含量显著下降(P<0。05);元素含量大小为:N>K>Ca>Fe>P>Mn>Mg>Cu>Zn。3)川黄檗对根际土壤中矿质元素的富集能力不同,对Ca、Mg的富集能力较强,对N、P和K的富集能力居中,对Fe、Mn和Cu的富集能力较低。4)叶中K与P,当年生枝及根中的N与K间均存在显著正相关(P<0。05),各部位N与多种元素相关性显著(P<0。05);土壤中元素与叶、根中多种元素显著相关(P<0。05)。[结论]川黄檗幼龄林不同生长年限各部位及土壤中矿质元素含量呈现不同的变化规律,各部位元素之间及与土壤中矿质元素既有协同作用又有拮抗作用,不同部位对矿质营养元素具有不同的富集能力。依据研究结果,川黄檗幼龄林施肥时应该注意补充叶中N、Ca、Cu和Zn,同时合理搭配P和Mg等元素,注意用量的协调,保证植株营养均衡。
Analysis of mineral element content and correlation with rhizosphere soil factors in Phellodendron chinense of different ages
[Objective]This study aims to explore the patterns of mineral element content variation in different parts and rhizosphere soil of Phellodendron chinense of different ages.Additionally,it investigates the correlation between mineral elements and soil factors.The findings provide a basis for nutritional diagnosis and scientifically informed fertilization practices in young P.chinense.[Method]The contents and changes of mineral elements in different parts(leaf,current-year branch and root)and rhizosphere soil of P.chinense 1-3 a seedlings were studied.The correlation between rhizosphere soil and different parts,as well as between mineral elements in each part,was analyzed,and the enrichment ability of different parts to mineral nutrients in soil was evaluated.[Result]1)Significant variations were observed in mineral element content among different tree ages and parts.With increasing tree age,the content of N,Ca,Cu,Zn in leaf,P and Cu in current-year branch,and Mg in root showed a significant decrease(P<0.05).2)Significant differences were found in the mineral element content of rhizosphere soil among different tree ages(P<0.05).Ca,Mn,and Zn content significantly increased with tree age(P<0.05),whereas Fe content exhibited a significant decrease(P<0.05).The order of mineral element content in rhizosphere soil was:N>K>Ca>Fe>P>Mn>Mg>Cu>Zn.3)P.chinense had different enrichment capacity for mineral elements in rhizosphere soil,with strong enrichment capacity for Ca and Mg,medium enrichment capacity for N,P and K,and low enrichment capacity for Fe,Mn and Cu.4)Significant positive correlations were observed between K in leaf and P(P<0.05),as well as between N in current-year branch and root with K.N in various parts showed significant correlations with multiple elements(P<0.05).Furthermore,significant correlations existed between soil elements and multiple elements in leaf and root(P<0.05).[Conclusion]The contents of mineral elements in different parts of young forest of P.chinense and soil in different growing years show different changing regularity.There are both synergistic and antagonistic effects between elements in different parts and with mineral elements in the soil,and different parts have different enrichment ability to mineral nutrient elements.These findings suggest the need to supplement N,Ca,Cu,and Zn in leaf and ensure a balanced application of P and Mg when fertilizing young P.chinense to maintain optimal nutrient balance in plants.

Phellodendron chinensedifferent organsrhizosphere soilmineral elementscorrelation analysisenrichment characteristics

孙志鹏、罗建勋、王刚

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四川省林业科学研究院 森林和湿地生态恢复与保育四川省重点实验室,四川 成都 610081

四川农业大学 林学院,四川 成都 611800

川黄檗 不同部位 根际土壤 矿质元素 相关性分析 富集特征

四川省重点研发计划

2021YFN0110

2024

中南林业科技大学学报
中南林业科技大学

中南林业科技大学学报

CSTPCD北大核心
影响因子:1.442
ISSN:1673-923X
年,卷(期):2024.44(3)
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