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为探究计划烧除对云南松林土壤水文特征的影响,为计划烧除后森林生态系统服务功能评价提供依据,以云南省新平县实施多年计划烧除的云南松纯林为研究对象,设立20 m×20 m计划烧除样地和不进行计划烧除的自然对照样地各3块。2019年2月实施计划烧除作业,进行样地调查、火烧强度和枯落物储量调查,2020年6月采集土样,测定土壤物理、化学性质和土壤入渗性能。结果表明,计划烧除后土壤容重增加且在0~10 cm土层差异显著;毛管孔隙度和总孔隙度减少但差异不显著;有机质减少并在0~20 cm土层差异显著。计划烧除后土壤自然含水率、饱和持水率、毛管持水率和田间持水量减少但差异不显著;吸湿水量减少并且在0~20 cm土层差异显著。计划烧除后土壤初渗速率、土壤平均入渗速率和土壤稳定入渗率减少;土壤初渗速率和平均入渗速率在不同样地0~20 cm土层差异显著。计划烧除对土壤稳定入渗率的显著影响因素为土壤容重、孔隙度、有机质和饱和持水率。说明计划烧除后云南松林土壤持水性能下降,入渗性能下降,对于入渗性能的影响主要是源于土壤理化性质的改变。 相似文献
3.
Satyam Verma 《Journal of Sustainable Forestry》2018,37(7):678-690
The role of forest fires in the soil dynamics and global carbon cycle has not been comprehensively studied in tropical forests as the effects of fire on tropical forest soils can be extremely variable. This study was aimed to understand how repeated fires affect physical and chemical properties of soil in a tropical dry deciduous forest and alter soil fertility and health. The study was carried out in the dry deciduous forest of Mudumalai Tiger Reserve. Soil samples were collected from unburned (B0) to six-time burned (B6) plots. Samples were collected from each plot from three different depths viz. 0–10 (Top), 10–20 (Middle), and 20–30 cm (Bottom) and analyzed for soil physical and chemical properties. Soil pH, EC, WHC decreased with increasing fire frequencies while bulk density increased. Organic Carbon, Total N, and available P decreased with increasing fire frequencies whereas extractable K initially increased but decreased with the very high frequency of fires. NO3?N slightly decreased with high fire frequencies but NH4?N decreased significantly with increasing fire frequency. These results provide a new insight regarding the influence of repeated fires on soil that will be valuable to understand the effect of fire on the recovery of soils and nutrient dynamics. 相似文献
4.
The species composition and diversities, and soil properties under canopy gaps in broad-leaved Pinus koraiensis forests were studied in the Changbai Mountains. The results indicated that the species composition and diversities in gap
were different from those under canopy. The Shannon-Wiener index, evenness index, and abundance index in gap were higher than
those under canopy in the seedling layer, while the community dominance in the seedling layer increased in closed canopy.
The physicochemical properties of soil changed with the change of space and resource availability in gaps. The thickness,
standing crop, and water holding capacity of the litter layer under canopy were significantly (p<0.01) higher than those in gap. The content of total nitrogen and total potassium of litter in gap were 10.47% and 20.73%
higher than those under canopy, however, the content of total phosphorus and organic carbon under canopy were 15.23% and 12.66%
more than those under canopy. The water content of 0–10 cm and 10–20 cm of soil layer in gap were 17.65% and 16.17% more than
those under canopy. The soil buck density of 0–10 cm were slightly higher under canopy than that in gaps, but there was no
significant difference in the soil buck density of the 10–20 cm soil layer. The soil pH values were 5.80 and 5.85 in gap and
under canopy, respectively, and were not significantly different. The content of soil organic matter, total nitrogen, and
total potassium in gap were 12.85%, 7.67%, and 2.38% higher than those under canopy. The content of NH4
+-N, available phosphorus, available potassium, and total phosphorus in soil under canopy were 13.33%, 20.04%, 16.52%, and
4.30% higher than those in gap.
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Translated from Forest Research, 2006, 19(3): 347–352 [译自: 林业科学研究] 相似文献
5.
Microbial community functional diversity is a sensitive indicator of soil.Forest fires can change microbial community functional diversity.In this research,the fired soil samples were collected from Huzhong of Daxing’anling in Heilongjiang Province. The functional diversity of soil microbial community was detected by BIOLOG system.The average well color development(AWCD) in BIOLOG plates indicated the ability of carbon substrate utilization of microbial community.The indices of Shannon, Simpson and Mcintosh were calculated to show the richness,dominance and evenness of the functional diversity,and the principal component analysis of substrate reactions reflected the main carbon sources utilized by microbial community.The results showed that all the samples exhibited the reduction of AWCD during the first 144 hours of incubation,but there were obvious differences in the reduction degree among the samples.All kinds of fire intensities could influence microbial community functional diversity. The low fire intensity increased the richness (Shannon),dominance(Simpson) and evenness (Mcintosh) of microbial community.However,the intermediate and high fire intensity reduced these parameters,suggesting that the burned soil emitted gaseous nitrogen,a number of organic carbon and available phosphorus,which caused the reduction of the microorganism in quantity and type,and change in soil ingredients.The organic material reduced in the burned soil,in the same time,the pH values rose,which changed environment in which microorganism lives.The changed environment might not be conducive to activities of the microorganism.The principal component analysis showed that the main carbon sources for soil microbes were carbohydrates and amino acids and the carbon substrate utilization patterns in different samples were significant different.The results indicated that functional diversity of soil microbes were altered by forest fires,and the ability of microbes to utilize carbon source and the type of carbon sources were affected by dif 相似文献
6.
不同林火强度对大兴安岭偃松林土壤微生物功能多样性的影响 总被引：2，自引：0，他引：2
采用BIOLOG方法研究黑龙江省大兴安岭地区呼中林区不同林火强度对土壤微生物功能多样性的影响。在培养144h达到对数增长期的土样中,土壤微生物的碳源利用率因不同林火强度火烧而不同。高、中、低火烧强度均影响微生物群落多样性,特别是低强度火烧能提高微生物物种丰富度(Shannon指数)、物种优势度(Simpson指数)及群落均匀度(McIntosh指数);而中、高强度火烧使指数降低,这可能是由于土壤经过高温高热的灼烧,挥发了大量的气态氮、有机碳、速效磷,使火烧后土壤中的微生物数量、多样性锐减,并使成分发生改变,土壤中的有机质含量减少,同时,火后土壤的pH值升高,使微生物生存环境发生了变化,不利于微生物的活动。主成分分析表明:不同处理土壤微生物主要利用氨基酸类和糖类碳源,但不同火烧强度对微生物群落在碳源的利用上存在着较大的差异。林火可以改变土壤微生物功能多样性,不同林火强度使土壤微生物群落在碳源利用能力、利用类型以及群落的多样性上产生了较大的分异。 相似文献
7.
Long term effects of fire on ectomycorrhizas and soil properties in Nothofagus pumilio forests in Argentina 总被引：1，自引：0，他引：1
The forests of Nothofagus pumilio have historically been affected by forest fires. The effects of fire on certain above and belowground, biotic and abiotic components of these ecosystems have been previously documented, albeit belowground components have received much less attention. It has been suggested that the effects observed in the short-term after a fire usually differ from the longer-term effects. The long-term effects of fire (i.e. >5 years after burning) on belowground components in Nothofagus forests are currently unknown. In the present study we evaluated the long-term effect of fire on ectomycorrhiza (ECM) colonization and morphotype composition in N. pumilio roots, as well as soil chemical properties in temperate forests in Patagonia. Sampling was conducted in three mature monospecific forests. In each, nearby burned and unburned sites were selected. The time since the occurrence of fires differed between areas (i.e. 6-10 years). Within each site, 3 transects of 40 m were established randomly along which 5 samples of roots and soil were collected in spring and autumn. The main results were: (1) in comparison with the unburned site, ECM colonization was lower in the burned site in the area with the shorter time length since fire occurrence and no effects in the other two areas were observed; (2) richness and diversity were not significantly affected by fire but there was a significant effect of season for both parameters, being higher in spring; (3) ECM dominance was significantly higher in the unburned than in the burned site in Tronador, while in Challhuaco the opposite was observed, mainly in autumn; (4) in general carbon, nitrogen and phosphorous decreased while pH increased in the burned sites; (5) ECM colonization positively correlated with NH4+ and phosphorus and negatively with pH but was not significantly correlated with organic matter or any other soil variable. Altogether the results suggest that effects of fire on ectomycorrhiza and soil properties in N. pumilio forests are probably related to the time elapsed since fire occurrence combined with site characteristics. In addition, the direct and indirect effects of fire in these forest systems may persist for more than 10 years. 相似文献
8.
On some landscapes periodic fire may be necessary to develop and maintain oak-dominated savannas. We studied the effects of two annual prescribed burns to determine their effect on microbial activity and soil and litter nutrients 1 year after the last burn. Surface litter and soil from the upper 0–5 cm soil layer in three developing savannas (oak-hickory, Quercus-Carya), oak-hickory-pine (Quercus-Carya-Pinus), and pine (Pinus) were collected one year after the second of two annual prescribed burns. Surface litter was analyzed for nutrients and soil was analyzed for phospholipid fatty acids (PLFAs) and nutrients. Surface litter chemistry differed across the three savannas for potassium (K) and boron (B), being significantly (P < 0.05) higher for unburned forest than for burned forest. Among savannas, only sulfur (S) was higher for the pine savanna and B for the oak-hickory savanna, both were higher for unburned forest than for burned forest. For soil, calcium (Ca) and B differed across savannas, being higher for burned forest than for unburned forest. Among savannas, soil pH, Ca, and B concentrations were higher in soil from burned forest than from unburned forest. Total PLFA differed among savannas, but was not affected by burning treatments. However, the amounts of biomarkers for Gram-positive and Gram-negative bacteria were higher while the amount of biomarker for fungal PLFA was lower for burned forest than for unburned forest. Our results indicate that the two annual prescribed burns moderately affected PLFA microbial community structure and litter and soil nutrient concentrations. However, the long-term effects of fire on these study sites are not known and merit further study. 相似文献
9.
Wildfire can create a mosaic of impacts of varying severity across the landscape. Although widely recognized, this feature
and its causes are little understood or studied in ecology. We studied a 1,200-ha wildfire in the southern boreal forest of
the Boundary Waters Canoe Area Wilderness (BWCAW) in northeastern Minnesota, USA, using 275 ground plots (stand-scale) and
1:7,000 scale aerial photographs for the entire burned area (landscape-scale). Fire severity was markedly heterogeneous. Overall,
50% of the burn extent was classified as high burn severity, but patches burned this severely were on average less than 70 m
from patches of low severity. As expected, lowlands had lower average fire severity than uplands, but several lowland areas
burned, and some upland areas remained unburned. At the landscape scale, pre-fire vegetation type—itself heterogeneous—and
patch size of less flammable cover types influenced fire severity. Crown fire severity in upland areas was lowest in pure
aspen–birch and red/white pine stands and highest in jack pine and spruce–fir stands. At the stand-scale, slope position and
the density of certain tree species at adjacent plots influenced fire severity. Improved understanding of the severity patterns
created by wildfire can help to guide the management of spatial patterns of forested systems. Based on our study, a larger
range in disturbance severity at scales of 0.1 to several ha and increasing the average size, and range of sizes, of residual
patches would in aggregate better mimic natural disturbance than typical harvests. 相似文献
10.
中度火干扰对白桦落叶松混交林土壤理化性质的影响 总被引：10，自引：0，他引：10
应用空间代替时间的方法对大兴安岭林区白桦落叶松混交林1982-2007年的中度火烧迹地土壤理化性质变化进行研究.结果表明:火后土壤密度增加,土壤孔隙度和土壤含水率降低,但是变化幅度将随着时间的推移逐渐缩小,并在火烧后第20年将接近火烧前水平;火烧后A层和B层土壤有机质均呈降低趋势,A层的降幅逐渐缩小直到火烧后20年比火烧前水平大幅增加;火后土壤A层和B层全磷含量均呈增加趋势,土壤全氮在A层基本也呈增加趋势,B层随火后时间呈波动变化,无明显规律;土壤有效磷含量变化星先降低后增加的趋势;A层土壤速效钾含量的变化基本呈增加趋势,但随时间增加幅度减小,而B层的变化无规律;A层土壤水解氮含量变化呈增加趋势,而B层的变化则与速效钾在B层的变化相似,无明显规律.此研究旨在找出火烧后随时间的推移土壤理化性质的动态变化规律,为火烧迹地的改造和生态恢复提供科学依据. 相似文献
11.
In order to clarify the effects of a mixture of deciduous broad-leaved trees on soil fertility, we investigated litter biomass
accumulation, mineral soil chemical and physical characteristics, characteristics of nitrogen mineralization, and the mutual
relationships between them in Japanese cypress (Chamaecyparis obtusa) stands mixed with deciduous broad-leaved trees at different ratios (mixture ratio; MR = 0, 16, 33, 43, 100% by basal area)
in the northern Kanto region of Japan. Litter biomass in the forest floor and mineral soil was 19.1 Mg ha−1 in MR 0% and decreased approximately 60 % in MR 33%, MR 43% and MR100%. The permeability at 0–5 cm soil depth in MR100% was
twice as much as that in MR 0%. Increases in soil permeability were likely due to larger soil pores in the higher MR with
much accumulated deciduous broad-leaves. At 0–5 cm soil depth, the differences in carbon concentration among the plots were
not clear. On the other hand, carbon concentrations at 5–10 cm depth increased from 90 g kg−1 to 147 g kg−1 with increases in MR from 0% to 100%. Concentrations of exchangeable bases increased two to four times with increases in
MR from 0 to 100% at 0–10 cm depth. Soil pH (H2O) generally increased with increases in MR at each depth. The rates of net nitrogen mineralization at 0–5 cm depthin vitro increased from 25 to 87 mg kg−1 2 weeks−1 with increases in MR from 0 to 100%. However, increases in nitrification with increases in MR were not clear compared with
nitrogen mineralization. These results indicated that a mixture of deciduous broad-leaved trees in a Japanese cypress stand
was effective in preventing soil fertility decline.
This study was supported by a grant from the Showa Shell Sekiyu Fundation for Promotion of Environmental Research. A part
of this study was presented at the 7th International Congress of Ecology (1998). 相似文献
12.
Microenvironmental heterogeneity of soil physical properties in 0–20 cm and 20–40 cm soil layers in a broad-leaved Pinus koraiensis forest gap in Xiao Xing’anling Mountains were analyzed by geostatistical method. The results show that the amount of soil
water, saturation water capacity, capillary water capacity and porosity in the top layer were greater than those in the lower
layer, except for bulk density, where the opposite applied. Soil physical properties in the top soil layer had relatively
higher ranges and coefficients of variation. The total and auto correlation spatial heterogeneity of soil physical properties
in the top layer were larger than those in the lower layer. The soil water had a strong anisotropic structure in an easterly
and northerly direction, but porosity shows isotropy in the same directions. With increasing spatial distance, the other three
physical factors exhibited anisotropic structures. The mutual effect between semi-variograms of soil physical properties in
the top layer within the spatial autocorrelation range was not significant. For spatial distribution of physical properties
within different layers, the patches at the middle and lower ranks in the forest gap dominated. Patches at higher rank were
only distributed in the 0–20 cm soil layer and were located north of the forest gap center.
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Translated from Science of Soil and Water Conservation, 2007, 5(3): 52–58 [译自: 中国水土保持科学] 相似文献
13.
Over a period of 16 years, unburned longleaf pine (Pinus palustris Mill.) pole stands grew an average of 27% more volume than similar stands regularly burned. Treatments included biennial burns in winter, spring, and summer plus an unburned check, each of which was combined with three supplemental treatments, namely, initial herbicide injection of all hardwoods, repeated handclearing of all woody stems, and no treatment. All unburned and winter-burned plots were paired to study this growth reduction relative to treatments. The status of nitrogen, phosphorus, available moisture holding capacity, bulk density, and macropore space was determined in both surface and subsurface soils. Foliage from pines on sampled plots was analyzed for N, P, K, Ca, Mg, Mn, Cu, Fe, and Zn. Burning did not significantly affect either soil N and P or foliar nutrients. However, burning reduced available moisture holding capacity and macropore space and increased the bulk density of surface soils, and also reduced the moisture-holding capacity of subsurface soils. The results from this and other studies suggest that growth losses are due, at least in part, to increased moisture stress associated with changes in soil physical properties. 相似文献
14.
Morteza Pourreza Seyed Mohsen Hosseini Ali Akbar Safari Sinegani Mohammad Matinizadeh Seyed Jalil Alavai 《林业研究》2014,25(1):113-120
Zagros forests are mainly covered byQuercus brantii L. coppices and oak sprout clumps occupy the forest area like patches. We investigated post-fire herbaceous diversity in the first growing season after fire. For this purpose neighboring burned and unburned areas were selected with the same plant species and ecological conditions. The data were collected from areas subjected to different fire severities. Overall 6 treatments were considered with respect to fire severity and the mi-crosites of inside and outside of oak sprout clumps including： unburned inside and outside of sprout clumps （Ni and No）, inside of sprout clumps that burned with high fire severity （H）, inside of sprout clumps that burned with moderate fire severity （M）, outside of sprout clumps that burned with low fire severity （OH and OM）. Different herbaceous com-position was observed in the unburned inside and outside of oak sprout clumps. The species diversity and richness were increased in treatments burned with low and moderate fire severity. However, in treatment burned with high fire severity （H）, herbaceous cover was reduced, even-ness was increased, and richness and diversity were not significantly changed. We concluded that besides the microsites conditions in forest, fire severity is an inseparable part of the ecological effect of fire on her-baceous composition. 相似文献
15.
Snags are an important resource for a wide variety of organisms, including cavity-nesting birds. We documented snag attributes in a mixed-conifer forest dominated by ponderosa pine in the Sierra Nevada, California where fire is being applied during spring. A total of 328 snags were monitored before and after fire on plots burned once, burned twice, or left unburned to assess the effects of prescribed fire on snag populations. The greatest loss of snags (7.1 snags ha−1 or 43%) followed the first introduction of fire after a long fire-free period. On plots burned a second time 21% of snags (3.6 snags ha−1) were lost, whereas 8% (1.4 snags ha−1) were lost on unburned control plots in the same time period. New snags replaced many of those lost reducing the net snag losses to 12% (2.0 ha−1) for plots burned once, and 3% (0.5 ha−1) for plots burned twice and unburned plots. We also examined snags used by cavity-nesting birds. Snags preferred for nesting were generally ponderosa pine (Pinus ponderosa), larger diameter, and moderately decayed as compared to available snags. For monitored snags that met the preferred criteria, there was a net loss (1.7 snag ha−1 or 34%) after the first burn, while the loss of useable snags was less than 1 snag ha−1 following the second burn (15%) or on unburned controls (8%). We recommend protection of preferred snags, in particular large ponderosa pines, especially during primary fire applications on fire-suppressed landscapes. 相似文献
16.
在滇中安宁“3·29”重大森林火灾火烧迹地选择无人为干扰的灌木林设置样地,并与未过火的灌木林进行比较,通过外业调查和实验室测定,研究了可燃物的种类、高度、绝对含水量、载量等特征。结果表明,火烧迹地死可燃物的高度为5．7m,与未过火的活灌木高度5．4m差不多,活灌木平均高度达1．5m;火烧迹地活灌木、死可燃物、CWD的热值及点着温度与未过火样地的差异均不明显;火烧迹地CWD的灰分含量仅为未过火的25．87％;火烧迹地总的可燃物载量为9．07kg/m^2,明显超过了未过火样地7．82kg／m^2。 相似文献
17.
林火对土壤氮含量的扰动作用 总被引：3，自引：0，他引：3
通过对大兴安岭地区新林林业局 2 0a内不同年份间隔的 11块火烧迹地土壤进行调查取样和室内实验分析 ,发现火烧后不同年限、不同强度的火烧迹地 ,土壤全氮与有效氮含量变化情况如下 :低强度火烧后 9d ,土壤全氮和有效氮含量均比未烧前低 ,这与中、高强度火烧后的情况正好相反。火烧后 4a内 ,土壤氮的含量基本都比未烧林地有所下降 (中强度火烧迹地土壤有效氮含量除外 )。以后有逐年增加的趋势。火烧迹地降第一场雨后 ,低强度火烧迹地土壤全氮比降雨前减少 ,有效氮增加 ;中强度火烧迹地土壤全氮和有效氮均比降雨前增加 ;高强度火烧迹地土壤全氮和有效氮均比降雨前有所下降。连年火烧迹地土壤全氮减少 ,有效氮增加 相似文献
18.
Fire affects the physical and chemical properties and soil biological activity of natural ecosystems. This study was conducted in the Miyan Tang region, Ilam Province in western Iran. The study site was 110 hectares, where we sampled soils in areas that were classified by fire severity: low (LS), high (HS) and medium severity (MS), and unburned (UB), which served as the control. In each severity class, 25 transect points were randomly selected for measurement. Around each transect plot center, 3 soil samples were selected randomly and soils collected from the 0 to 20 cm depth were combined into a composite sample that was used in laboratory analysis to represent conditions at that point. Plots in the UB and LS fire classes had similar soil conditions and had higher values of factors such as saturated moisture, organic carbon, carbon dioxide, and silt and clay content. In contrast, plots in the HS and MS fire severity classes were clustered in the positive direction along the first axis that represented gradients in soil acidity, electrical conductivity, cation exchange capacity, accessible phosphorus, accessible potassium, bulk density, and sand. Soil attributes were similar in areas of HS and MS fire severity classes, whereas soil conditions in the LS class and UB controls were most similar. Fire in the LS areas either did not significantly alter the physical–chemical soil properties and microbial basal respiration, or soils were able to recover quickly after being burned. 相似文献
19.
The soil microbial biomass and nutrient status under the native broadleaved forest and Cunninghamia lanceolata plantations at the Huitong National Research Station of Forest Ecosystem (in Hunan Province, midland of China) were examined
in this study. The results showed that after the native broadleaved forest was replaced by mono-cultured C. lanceolata or C. lanceolata, soil microbial biomass and nutrient pool decreased significantly. In the 0–10 cm soil layer, the concentrations of soil
microbial carbon and nitrogen in the broadleaved forest were 800.5 and 84.5 mg/kg, respectively. These were 1.90 and 1.03
times as much as those in the first rotation of the C. lanceolata plantation, and 2.16 and 1.27 times as much as those in the second rotation of the plantation, respectively. While in the
10–20 cm soil layer, the microbial carbon and nitrogen in the broadleaved forest were 475.4 and 63.3 mg/kg, respectively.
These were 1.86 and 1.60 times as much as those in the first rotation, and 2.11 and 1.76 times as much as those in the second
rotation, respectively. Soil nutrient pools, such as total nitrogen, total potassium, NH4
+-N, and available potassium, also declined after the C. lanceolata plantation replaced the native broadleaved forest, or Chinese fir was planted continuously. Less litter and slower decay
rate in pure Chinese fir plantation were the crucial factors leading to the decrease of soil microbial biomass and nutrient
pool in this area. Human disturbance, especially slash-burning and site preparation, was another factor leading to the decrease.
There were significant positive correlations between soil microbial carbon and nitrogen and soil nutrients. To improve soil
quality and maintain sustainable productivity, some measures, including planting mixed conifer with hardwood, preserving residues
after harvest, and adopting scientific site preparation, should be taken.
Translated from Chinese Journal of Applied Ecology, 2006, 17(12): 2,292–2,296 [译自: 应用生态学报] 相似文献
20.
Active organic carbon in soil has high biological activity and plays an important role in forest soil ecosystem structure and function. Fire is an important disturbance factor in many forest ecosystems and occurs frequently over forested soils. However, little is known about its impact on soil active organic carbon (SAOC), which is important to the global carbon cycle. To investigate this issue, we studied the active organic carbon in soils in the Larix gmelinii forests of the Da Xing’an Mountains (Greater Xing’an Mountains) in Northeastern China, which had been burned by high-intensity wildfire in two different years (2002 and 2008). Soil samples were collected monthly during the 2011 growing season from over 12 sample plots in burned and unburned soils and then analyzed to examine the dynamics of SAOC. Our results showed that active organic carbon content changed greatly after fire disturbance in relation to the amount of time elapsed since the fire. There were significant differences in microbial biomass carbon, dissolved organic carbon, light fraction organic carbon, particulate organic carbon between burned and unburned sample plots in 2002 and 2008 (p < 0.05). The correlations between active organic carbon and environmental factors such as water content, pH value and temperature of soils, and correlations between each carbon component changed after fire disturbance, also in relation to time since the fire. The seasonal dynamics of SAOC in all of the sample plots changed after fire disturbance; peak values appeared during the growing season. In plots burned in 2002 and 2008, the magnitude and occurrence time of peak values differed. Our findings provide basic data regarding the impact of fire disturbance on boreal forest soil-carbon cycling, carbon-balance mechanisms, and carbon contributions of forest ecosystem after wildfire disturbance. 相似文献