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中南林业科技大学林学院,长沙,410004
Published:2019
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LIU Falin, CHEN Xiaowei, ZENG Suping. Effects of Fire Disturbance on Soil Physiochemical Properties in[J]. 2019, 33(5): 132-138.
LIU Falin, CHEN Xiaowei, ZENG Suping. Effects of Fire Disturbance on Soil Physiochemical Properties in[J]. 2019, 33(5): 132-138. DOI: 10.13870/j.cnki.stbcxb.2019.05.020.
火干扰是影响森林土壤生态系统结构与功能的重要因素之一。探讨火干扰后森林土壤理化性质的动态特征,为火后植被恢复以及森林可持续经营提供重要的理论指导。2014-2016年在湖南省株洲市枫香次生林内设置16块20 m×20 m样地进行试验,研究4种火干扰强度(对照、低强度、中强度、高强度火烧)后不同时间节点(火烧后3,30,180,360,720天)的枫香次生林的土壤容重(BD)、土壤斥水性(SWR)、有机质(SOM)、pH、全氮(TN)、全磷(TP)和全钾(TK)等指标。通过描述性统计、单因素方差分析和Fisher LSD检验研究了土壤性质在同一时间节点不同火干扰强度之间以及同一火干扰强度下不同时间节点间的显著性差异(p<0.05)。结果表明:火干扰后各时间节点下,BD、SWR、pH、TK均随火强度增大而增加,而SOM和TP随火强度增大而降低,不同火干扰间TN均不存在显著性差异。同一时间节点内火干扰土壤与对照相比,低强度火干扰对BD、SWR、pH和SOM的影响不显著,中强度火对部分时间节点下的土壤理化性质有影响,而高强度火对其影响均比较显著。同一强度火干扰后,BD、SWR、pH在不同时间节点间存在显著性差异,BD、SWR、pH在火烧后3天显著增大,然后逐渐减少;BD在火后360天恢复到火烧前状态,而SWR、pH则需720天。SOM仅在高强度火烧后360,720天与其他时间节点间存在显著性差异;火干扰后,SOM与火烧前相比先减少,后逐渐上升,火后360天逐渐恢复到火烧前的水平并维持稳定。中、高强度火干扰后,时间节点跨度越大,TK的差异越显著,而TN和TP仅在高强度火烧后差异显著。研究发现火干扰强度和时间节点对7种土壤性质均有一定影响,其中高强度火干扰对土壤理化性质影响最大。火干扰后短期内引起地力衰退,影响林地土壤养分状况,对土壤生态系统产生重要影响,但随着时间推移,2年后土壤理化性质基本恢复到火烧前的水平。
Fire disturbance is one of the important factors affecting the structure and function of forest soil ecosystem. In order to provide theoretical guidance for forest regeneration and sustainable management after fire disturbance
this study explored the dynamic characteristics of physiochemical properties in forest soil after different fire disturbances. The effects of fire intensities (control
low
moderate and high intensity fire) and time nodes (3
30
180
360
720 days after fire) on bulk density (BD)
soil water repellency (SWR)
soil organic matter (SOM)
pH
total nitrogen (TN)
total phosphorus (TP) and total potassium (TK) contents were measured in a field-scale experiment with 16 plots (20 m×20 m) from Liquidambar formosana secondary forests in Zhuzhou
Hunan Province
China from 2014 to 2016. The differences and changing trends of soil properties among different fire disturbances at the same time node and different time nodes under the same fire disturbance were studied by descriptive statistical analysis
one way ANOVA and Fisher LSD test (p<0.05). The result showed that BD
SWR
pH
and TK increased with the increase of fire intensities
while SOM and TP decreased after the fire disturbance at the same time node. There was no significant difference of TN among different fire disturbances. Compared with the control
the effects of low intensity fire on BD
SWR
pH and SOM were not significant at the same time node
the effects of moderate intensity fire on these soil physiochemical properties were significant at some time nodes
while the effects of high intensity fire on them were significant. After the same intensity of fire disturbance
there were significant differences in BD
SWR and pH among different time nodes (p<0.05). BD
SWR and pH increased significantly at the first three days after fire
then decreased gradually; BD returned to pre-fire level after 360 days of fire
while SWR and pH needed 720 days after fire. However
there were significant differences of SOM between 360
720 days and other time nodes only after high intensity fire. After fire disturbance
SOM decreased first
then increased gradually
and returned to the level before fire and maintained stability after 360 days. After fire with moderate and high intensities
the greater the time span was
the more significant the difference of TK was
while the differences of TN
TP were only significant after high intensity fire. Fire intensities and time nodes had certain effects on the studied soil properties
among which high intensity fire showed the biggest effects on soil properties. Fire disturbance caused soil fertility decline in the short time and affected the soil nutrient status of forest land. However
with the time went on
the properties of soil physiochemical gradually recovered to the pre-fire level after two years.
Johnstone J F, Hollingsworth T N, Chapin F S, et al. Changes in fire regime break the legacy lock on successional trajectories in Alaskan boreal forest[J]. Global Change Biology,2010,16(4):1281-1295.
胡海清,刘洋,孙龙,等.火烧对不同林型下森林土壤水分物理性质的影响[J].水土保持学报,2008,22(2):162-165.
Certini G. Effects of fire on properties of forest soils:A review[J]. Oecologia,2005,143(1):1-10.
Banning N C. Murphy D V. Effect of heat-induced disturbance on microbial biomass and activity in forest soil and the relationship between disturbance effects and microbial community structure[J]. Applied Soil Ecology,2008,40(1):109-119.
Marafa L M, Chau K C. Effect of hill fire on upland soil in Hong Kong[J]. Forest Ecology and Management,1999,120(1/3):97-104.
Kutiel P, Naveh Z. The effect of fire on nutrients in a pine forest soil[J]. Plant and Soil,1987,104(2):269-274.
Kim Y, Tanaka N. Effect of forest fire on the fluxes of CO
2
, CH
4
and N
2
O in boreal forest soils, interior Alaska[J]. Journal of Geophysical Research,2003,108(1):1-12.
Blair J M. Fire, N availability, and plant response in grasslands:A test of the transient maxima hypothesis[J]. Ecology,1997,78(8):2359-2368.
Hatten J A, Zabowski D, Ogden A, et al. Soil organic matter in a ponderosa pine forest with varying seasons and intervals of prescribed burn[J]. Forest Ecology and Management,2008,255(7):2555-2565.
Kim Y S, Makato K, Takakai F, et al. Greenhouse gas emissions after a prescribed fire in white birch dwarf bamboo stands in northern Japan, focusing on the role of charcoal[J]. European Journal of Forest Research,2011,130(6):1031-1044.
张喜,朱军,崔迎春,等.火烧对黔中喀斯特山地马尾松林土壤理化性质的影响[J].生态学报,2011,31(19):5809-5817.
Baer S G, Kitchen D J, Blair J M, et al. Changes in ecosystem structure and function along a chronosequence of restored grasslands[J]. Ecological Applications,2002,12(6):1688-1701.
肖灵香,方晰,项文化,等.湘中丘陵区4种森林类型土壤理化性质[J].中南林业科技大学学报,2015,35(5):90-97.
谷会岩,金靖博,陈祥伟,等.不同火烧强度林火对大兴安岭北坡兴安落叶松林土壤化学性质的长期影响[J].自然资源学报,2010,25(7):1114-1121.
孙龙,赵俊,胡海清.中度火干扰对白桦落叶松混交林土壤理化性质的影响[J].林业科学,2011,47(2):103-110.
许舟,刘发林.马尾松林植物及土壤养分对频繁火干扰的响应[J].中南林业科技大学学报,2016,36(6):46-50.
Fischer G, Nachtergaele F, Prieler S, et al. Global agro-ecological zones assessment for agriculture (GAEZ 2008)[M]. ⅡASA, Laxenburg, Austria and FAO, Rome, Italy, 2008.
司绍兵.浅谈采伐迹地的炼山方法[J].安徽林业科技,2009(3):46-46.
Doerr S H, Dekker L W, Ritsema C J, et al. Water repellency of soils[J]. Soil Science Society of America Journal,2002,66(2):401-405.
中国土壤学会.土壤农业化学分析方法[M].北京:中国农业科技出版社,2000.
Xue L, Li Q J, Chen H Y. Effects of a wildfire on selected physical, chemical and biochemical soil properties in a
Pinus massoniana
forest in South China[J]. Forests, 2014,5(12):2947-2966.
辛颖,赵雨森,陈强.大兴安岭火烧迹地植被恢复后土壤理化性质[J].东北林业大学学报,2013,41(8):65-68.
Letey J. Causes and consequences of fire-induced soil water repellency[J]. Hydrological Processes, 2001, 15(15):2867-2875.
Mac Donald L H, Huffman E L. Post-fire soil water repellency[J]. Soil Science Society of America Journal,2004,68(5):1729-1734.
Gordillo-Rivero A J, Garcia-Moreno J, Jordan A, et al. Fire severity and surface rock fragments cause patchy distribution of soil water repellency and infiltration rates after burning[J]. Hydrological Processes,2014, 28(24):5832-5843.
Glenn N, Finley C D. Fire and vegetation type effects on soil hydrophobicity and infiltration in the sagebrush-steppe:I. Field analysis[J]. Journal of Arid Environments, 2010,74(6):653-659.
Robichaud P R, Hungerford R D. Water repellency by laboratory burning of four northern Rocky Mountain forest soils[J]. Journal of Hydrology,2000,231/232:207-219.
Hesammi E, Talebi A B, Hesammi A. A review on the burning of crop residue on the soil properties[J]. Walia Journal,2014,30(1):192-194.
Zhao Y, Wang Y Z, Xu Z H, et al. Impacts of prescribed burning on soil greenhouse gas fluxes in a suburban native forest of south-eastern Queensland, Australia[J]. Biogeosciences,2015,12(21):6279-6290.
赵彬,孙龙,胡海清,等.兴安落叶松林火后对土壤养分和土壤微生物生物量的影响[J].自然资源学报,2011,26(3):450-459.
Trabaud L. The effects of different fire regimes on soil nutrient levels in Quercus coccifera garrigue. In Mediterranean-Type Ecosystems[M]. Berlin:Springer, 1983:233-243.
Scharenbroch B C, Nix B, Jacobs K A, et al. Two decades of low-severity prescribed fire increases soil nutrient availability in a Midwestern, USA oak (
Quercus
) forest[J]. Geoderma,2012,183/184(8):80-91.
Wieting C, Ebel B A, Singha K. Quantifying the effects of wildfire on changes in soil properties by surface burning of soils from the Boulder Creek Critical Zone Observatory[J]. Journal of Hydrology:Regional Studies,2017,13(C):43-57.
刘瑞斌,李莉,陈鹏东,等.森林火灾对烟台蓁山次生林土壤性质的影响[J].生态环境学报,2016,25(8):1300-1305.
Bell R L, Binkley D. Soil nitrogen mineralization and immobilization in response to periodic prescribed fire in a loblolly pine plantation[J]. Canadian Journal of Forest Research, 1989, 19(6):816-820.
杨尚东,吴俊,谭宏伟,等.红壤区桉树人工林炼山后土壤肥力变化及其生态评价[J].生态学报,2013,33(24):7788-7797.
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