兴安落叶松林火烧迹地土壤有效磷与土壤微生物生物量磷时空演变特征
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国家自然科学基金项目(31870644);黑龙江省自然科学基金(LH2021C011)


Spatial and temporal evolution characteristics of soil available phosphorus and soil microbial biomass phosphorus in the burned area of Larix gmelinii
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The National Natural Science Foundation of China(31870644),The National Natural Science Foundation of Heilongjiang (LH2021C011)

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    摘要:

    野火是大兴安岭活跃的生态干扰因子,显著影响火烧迹地土壤有效磷(AP,Available Phosphorus)和土壤微生物生物量磷(MBP,Microbial Biomass Phosphorus),本文旨在了解兴安落叶松林火烧迹地AP、MBP的时空演变特征,并在此基础上探究两者间的偶联机制。采用"以空间换时间"的研究方法,于大兴安岭塔河地区兴安落叶松林火烧迹地选取实验样地,于未过火兴安落叶松林选取对照样地,踏查每个样地的海拔、坡度、坡向、坡位信息,测定火烧迹地土壤AP、MBP含量,分析兴安落叶松林火烧迹地AP与MBP的时空演变特征。火干扰后,火烧迹地土壤AP、MBP含量均随恢复时间表现出先减少后增加的趋势,恢复初期火烧迹地MBP含量显著低于未过火样地,AP含量显著高于未过火样地(P<0.05);不同海拔火烧迹地AP、MBP含量差异显著(P<0.05),不同海拔未过火样地AP、MBP含量均无显著差异(P>0.05)。火烧迹地土壤MBP、AP的随机森林回归模型的模型总解释度约为84%,而未过火样地的模型总解释度约为60%,两个模型均达到了极显著水平(P<0.001),在对照样地随机森林回归模型中,坡位达到了显著水平(P<0.05),坡向、坡度、海拔三个地形因子达到了极显著水平(P<0.01),在火烧迹地随机森林回归模型中,所有解释变量均达到了极显著水平(P<0.01)。火干扰对土壤微生物的影响是一个长期过程,相较于AP,MBP对火干扰的响应更为敏感。火干扰会显著加强地形因子对AP、MBP的影响力,并改变地形因子对AP、MBP影响力的相对重要性。

    Abstract:

    Wildfire is a common natural disturbance agent in the Greater Khingan Range that significantly affects soil available phosphorus (AP) and soil microbial biomass phosphorus (MBP) in the burned area. This study aims to assess spatial and temporal changes of the AP and MBP in the burned area of Larix gmelinii. On this basis, the relationship between AP and MBP is further explored. Using the research method of "space-for-time substitution", we established a 28-year fire chronosequence with 80 sites over a small region of the Greater Khingan Range, selected three replicated plots in each burned area, and selected the nearby unburned area as the control plots. We measured the soil AP and MBP contents and topographic factors (altitude, slope position, slope aspect, slope gradient) for each plot. We analyzed the temporal and spatial evolution characteristics and the laws of AP and MBP in the burned area of Larix gmelinii. On this basis, the associated mechanisms of MBP and AP in the burned area of Larix gmelinii is further explored. After the fire disturbance, the contents of AP and MBP in the burned area initially decreased and then increased with the recovery time. In the initial stage of restoration, the MBP content of the burned area was significantly less than that of the unburned area, while the content of AP was significantly higher than that of the unburned area (P<0.05). The differences of AP and MBP contents in the burned area at different altitudes were significant (P<0.05), the differences of AP and MBP contents in the unburned area at different altitudes were not significant (P>0.05). The total explanatory power of the random forest regression model of soil MBP and AP in the burned area is about 84%, while that of the unburned area is about 60%, both models have reached an extremely significant level (P<0.001). In the random forest regression model of the unburned area, the slope position reached a significant level (P<0.05), the slope aspect, slope gradient, and altitude reached an extremely level (P<0.01). In the random forest regression model of the burned area, each explanatory variable reached an extremely level (P<0.01). The influence of fire disturbance on soil microorganisms is generally a long-term process and MBP is more sensitive than AP to fire disturbance. Fire disturbance will significantly strengthen the influence of terrain factors on AP and MBP, and change the relative importance of terrain factors on AP and MBP.

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杨光,李兆国,石炳东.兴安落叶松林火烧迹地土壤有效磷与土壤微生物生物量磷时空演变特征.生态学报,2023,43(12):5027~5037

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