罗斯生, 罗碧珍, 魏书精, 等. 森林火灾对马尾松次生林土壤活性有机碳的影响[J]. 西南林业大学学报(自然科学), 2021, 41(5): 121–130 . DOI: 10.11929/j.swfu.202009007
引用本文: 罗斯生, 罗碧珍, 魏书精, 等. 森林火灾对马尾松次生林土壤活性有机碳的影响[J]. 西南林业大学学报(自然科学), 2021, 41(5): 121–130 . DOI: 10.11929/j.swfu.202009007
Luo Sisheng, Luo Bizhen, Wei Shujing, Hu Haiqing, Song Hong, Wu Zepeng, Wang Zhenshi, Zhou Yufei, Li Xiaochuan, Zhong Yingxia, Li Qiang. Effects of Forest Fires on Soil Labile Organic Carbon in Secondary Forest of Pinus massoniana[J]. Journal of Southwest Forestry University, 2021, 41(5): 121-130. DOI: 10.11929/j.swfu.202009007
Citation: Luo Sisheng, Luo Bizhen, Wei Shujing, Hu Haiqing, Song Hong, Wu Zepeng, Wang Zhenshi, Zhou Yufei, Li Xiaochuan, Zhong Yingxia, Li Qiang. Effects of Forest Fires on Soil Labile Organic Carbon in Secondary Forest of Pinus massoniana[J]. Journal of Southwest Forestry University, 2021, 41(5): 121-130. DOI: 10.11929/j.swfu.202009007

森林火灾对马尾松次生林土壤活性有机碳的影响

Effects of Forest Fires on Soil Labile Organic Carbon in Secondary Forest of Pinus massoniana

  • 摘要: 以广东省鹤山市马尾松次生林为研究对象,在实地调查采样和室内试验的基础上,开展森林火灾后土壤活性有机碳含量的测定、剖析森林火灾对土壤活性有机碳的影响。结果表明:相比对照,幼龄林、中龄林和成熟林的0~60 cm土壤活性有机碳组分依次降低18.50%~26.03%、17.81%~22.96%和13.50%~19.41%。土壤深度分别解释了土壤MBC、DOC、EOC和POC变异的70.73%、28.34%、79.83%和73.35%,林龄分别解释了土壤MBC、DOC、EOC和POC变异的20.09%、62.27%、13.92%和18.13%,森林火灾分别解释了土壤MBC、DOC、EOC和POC变异的4.69%、5.39%、2.61%和3.42%。马尾松次生林土壤活性有机碳各组分分配比例均随林龄增长呈现出先增加后减少的规律,其中土壤EOC的分配比例最大,幼龄林、中龄林和成熟林的分配比例分别为29.96%、33.29%和33.35%。在垂直方向上,森林火灾后马尾松次生林土壤MBC和EOC随着土壤深度加深而逐渐减小,而成熟林的土壤DOC则随着土壤深度加深呈现增大的趋势,土壤POC没有明显的变化规律。森林火灾均降低了马尾松次生林各林龄土壤活性有机碳各组分含量,且在垂直方向上,各林龄马尾松次生林土壤活性有机碳各组分含量的变化量均随土层深度加深而逐渐减小。

     

    Abstract: Taking the secondary forest of Pinus massoniana in Heshan City of Guangdong Province as the research object. Based on the field investigation, sampling and indoor test, soil labile organic carbon after forest fire were tested, and the content of soil labile organic carbon before and after forest fire were tested. The effect of forest fire on the content of soil labile organic carbon in secondary forest of P. massoniana was analyzed. The findings indicated that compared with the control, the soil labile organic carbon components of young forest, middle-age forest and mature forest decreased by 18.50–26.03%, 17.81–22.96% and 13.50–19.41%. Soil depth explained 70.73%, 28.34%, 79.83%, and 73.35% of soil MBC, DOC, EOC, and POC variations, respectively. Stand age explained 20.09%, 62.27%, 13.92% and 18.13% of soil MBC, DOC, EOC, and POC variations. Forest fires explained 4.69%, 5.39%, 2.61%, and 3.42% of soil MBC, DOC, EOC, and POC variations, respectively. The distribution proportion of each component of soil labile organic carbon in the secondary forest of P. massoniana increased first and then decreased with the increase of stand age, among which the distribution proportion of soil EOC was the largest, the distribution proportion of young forest, middle forest and mature forest were 29.96%, 33.29% and 33.35% respectively. In the vertical direction, the soil MBC and EOC of P. massoniana secondary forest decreased with the deepening of soil depth after the sudden forest fire, while the soil DOC of mature forest increased with the deepening of soil depth, and there was no obvious change rule of soil POC. Forest fires reduced the content of soil labile organic carbon components of P. massoniana secondary forest at different ages, and in the vertical direction, the changes of the content of soil labile organic carbon components of P. massoniana secondary forest at all ages decreased with soil depth.

     

/

返回文章
返回