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祁连山天涝池流域森林土壤中硒的分布及主要输入途径

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为了明确森林土壤中硒的分布情况及其主要的输入途径,选择祁连山中部寺大隆自然保护站的天涝池流域为研究区,以祁连圆柏林土壤为研究对象,分析各土壤层中硒的含量特征以及大气沉降和凋落物对土壤中硒的贡献,对土壤中硒的停留时间和积累增量进行预测。结果表明,祁连圆柏林土壤层中硒含量依次为枯枝落叶层<腐殖质层<矿物质层。整体上,随着海拔的升高,祁连圆柏林各土壤层中硒含量呈下降的趋势,但不显著。林内大气沉降中硒的年通量(823。80 μg/m2)大于林外(549。77 μg/m2);叶凋落物中硒的年通量为269。76 μg/m2。有机质层土壤中硒的平均停留时间为89 a。林内、外表层土壤中硒的含量在未来30 a迅速增加,此后增加幅度减缓。
Distribution and main input pathways of Se in forest soil in the Tianlaochi catchment of the Qilian Mountains
To clarify the distribution of Se in forest soil and its main input pathways,the study focused on the Tianlaochi catchment of the Sidalong Nature Conservation Station in the central part of the Qilian Mountains,with our research object being the soil of the Qilian juniper forest(QJF).The content of Se was analyzed in each soil horizon,as well as the contribution of atmospheric deposition and litter to soil Se.And the residence time and accumulation increment of Se in forest soils were predicted.The results showed that the Se content in the soil was increased in the order:litter horizon<humus horizon<mineral horizon.Se content in each soil layer of QJF showed a decreasing trend with increasing elevation,al-though this trend was not statistically significant.The annual flux of Se in atmospheric deposition inside the forest(823.80 μg/m2)was higher than that outside(549.77 μg/m2);the annual flux of Se in the needle litter of QJF was 269.76 μg/m2.The mean residence time of Se in the organic horizon soil of QJF was 89 a.The content of Se in the surface soil inside and outside QJF would rapidly increase in the next 30 a,and the increase rate would slow down thereafter.

Qilian juniperatmospheric depositionlitterresidence timeincrement predictionselenium

易玉媛、马建成、王若淳、王娇娇、赵传燕、臧飞

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甘肃祁连山国家级自然保护区管护中心 寺大隆自然保护站,甘肃 张掖 734000

兰州大学草地农业科技学院,兰州 730020

祁连圆柏 大气沉降 凋落物 停留时间 增量预测

2024

兰州大学学报(自然科学版)
兰州大学

兰州大学学报(自然科学版)

CSTPCD北大核心
影响因子:0.855
ISSN:0455-2059
年,卷(期):2024.60(6)