太行山区主要森林类型叶枯落物及土壤持水特性对郁闭度的响应OA
Responses of litterfall and soil hydrological effects of major forest types to canopy density in the Taihang Mountains
以太行山地区典型林分——油松(Pinus tabuliformis)、侧柏(Platycladus orientalis)和刺槐(Robinia pseudoacacia)为研究对象,通过浸水法、环刀法等方法研究了不同郁闭度下枯落物及土壤的持水特征.结果表明:(1)油松林枯落物储量最大,侧柏林枯落物储量次之,刺槐林储量最小.刺槐林枯落物储量变化范围为:2.9~4.3 t/hm2;侧柏变化范围为3.9~9.1 t/hm2;油松变化范围为5.9~13.1 t/hm2.表现为储量随郁闭度增加而增加.(2)枯落物未分解层和半分解层持水量与浸泡时间呈明显对数关系,半分解层持水效果优于未分解层,油松和侧柏在大于0.7郁闭度下枯落物持水能力最好,刺槐在0.4~0.7郁闭度下枯落物持水能力最强.3种林地枯落物最大持水率依次为:油松>侧柏>刺槐.(3)油松林和侧柏林随郁闭度增加土壤容重逐渐减小,孔隙度逐渐增大;刺槐林随郁闭度增加0~20 cm 土层土壤容重逐渐减小,孔隙度逐渐增大,20~40 cm 土层孔隙度逐渐减小.
In this study,the typical forest stands of Pinus tabuliformis,Platycladus orientalis and Robinia pseudoacacia in the Taihang Mountain area were taken as the research objects,and the water-holding characteristics of litterfall and soil under different canopy densities were studied by water immersion method and cutting ring method.The results showed that:(1)The litter storage of Pinus tabuliformis forest was the largest,followed by the litter storage of P.orientalis,and the smallest storage of Robinia pseudoacacia forest.The variation range of litter storage in Robinia pseudoacacia forest was 2.9~4.3 t/hm2,with that of 3.9~9.1t/hm2 in P.orientalis forest and 5.9~13.1 t/hm2 in Pinus tabuliformis forest.It is manifested that the reserve increases with the increase of canopy density.(2)There was an obvious logarithmic relationship between the water-holding capacity of the undecomposed layer and the semi-decomposed layer and the soaking time,and the water-holding capacity of the semi-decomposed layer was better than that of the undecomposed layer.The water-holding capacity of the litter was the best in Pinus tabuliformis and P.orientalis in the canopy density greater than 0.7,and the water-holding capacity of the litter was the strongest in the R.pseudoacacia forest under the canopy density of 0.4~0.7.The maximum water-holding capacity of litter in the three woodlands was as follows:Pinus tabuliformis>P.orientalis>Robinia pseudoacacia.(3)P.tabuliformis forest and P.orientalis gradually decreased with the increase of canopy density,and the soil bulk density gradually increased.With the increase of canopy density,the bulk density of the soil in the 0~20 cm soil layer gradually decreased,the porosity gradually increased,and the porosity of the 20~40 cm soil layer gradually decreased.
董欣然;柔叙伊;马长明
河北农业大学林学院,河北保定 071000河北农业大学林学院,河北保定 071000河北农业大学林学院,河北保定 071000
农业科技
枯落物土壤持水特征郁闭度
litterfallsoilwater-holding characteristicscanopy density
《林业与生态科学》 2026 (2)
19-27,9
"三北"工程区植被恢复关键技术创新与示范项目(2025JBGS0001).
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