长白山阔叶红松林表层土壤水分空间异质性的地统计学分析

采用时域反射仪对长白山原始阔叶红松林3块50 m×50 m样地表层土壤（0～7.5 cm）水分进行测定,应用地统计学的理论与方法对表层土壤水分的空间异质性进行分析.结果表明：研究区3块样地表层土壤水分变异系数分别为24.32%（样地1）、24.11%（样地2）和23.60%（样地3）,均属于中等变异性;该区表层土壤水分的理论变异模型为球状模型,具有高度的空间异质性,其空间异质性以空间自相关部分为主;表层土壤水分的结构比分别为57.9%（样地1,属中等相关性）、83.3%和90.0%（样地2和3,属强烈的空间相关性）;研究区表层土壤水分的变程在5.5～13.1 m,与贝叶斯方法估计的变程相差不大;通过克立格插值估计,研究区表层土壤水分含量的平均值分别为49.3%（样地1）、52.8%（样地2）和42.6%（样地3）.     

Invasion of the alien shrub Prunus laurocerasus in suburban deciduous forests: Effects on native vegetation and soil properties

Most invading alien plants affect native biodiversity and ecosystem functioning. In a field survey, we assessed the impact of the invasive shrub Prunus laurocerasus on the native vegetation and soil properties in suburban deciduous forests in the region of Basel, Switzerland. We installed four pairs of plots in patches of P. laurocerasus and in adjacent not invaded areas in each of twelve forest areas. Native species richness, Shannon-diversity and species composition of the ground vegetation and shrub layer were assessed in each plot. Furthermore, in each plot we measured physical and soil chemical characteristics, enzyme activities and the carbon source utilization pattern of the soil microbial community using Ecoplates™. The maximum age of P. laurocerasus in each plot was determined using tree ring analysis, indicating the time elapsed since the invasive plant has established. A lower native plant species richness in both the ground vegetation and shrub layer was observed in plots with presence of P. laurocerasus. A different species composition of the ground vegetation was also found among plots with and without the invasive shrub. Plots invaded by P. laurocerasus had a lower soil moisture content than control plots. The intensity, diversity and substrate richness of the carbon sources were increased in soil from invaded plots compared to soil in control plots. However, the chemical soil characteristics examined and the activities of enzymes were not influenced by the invasive plant. The effects of P. laurocerasus became more pronounced with the time elapsed since the invasive plant has established. Thus, the removal of young P. laurocerasus individuals would be an appropriate management practice for this invasive shrub species.     

放牧对鄂尔多斯高原油蒿草场生物量及植被-土壤碳密度的影响

以围封保护和自由放牧油蒿草场为研究对象,通过野外调查与室内分析,研究了围封和放牧条件下沙地草场生物量和植被-土壤碳密度。结果表明:(1)自由放牧使油蒿群落中植物种类增加,但降低了植物群落盖度。自由放牧不仅导致油蒿草场地上、地下总生物量降低,也使得油蒿地上、地下生物量占群落地上、地下总生物量的比例减小。生长季自由放牧样地凋落物生物量显著大于围封保护样地(P0.05);(2)围封保护样地植被碳密度大于自由放牧样地,土壤碳密度却小于自由放牧样地,但两个样地间差异不显著(P0.05);(3)油蒿草场90%以上的碳储存于土壤中,围封保护样地和自由放牧样地油蒿草场土壤碳密度占植被-土壤系统碳密度的91%、93%;(4)围封保护油蒿草场碳密度为2.29 kg/m2,自由放牧油蒿草场碳密度为2.68 kg/m2,两个样地间差异不显著,自由放牧对油蒿草场碳密度影响不大。     

Impact of Manure Fertilization on the Abundance of Antibiotic-Resistant Bacteria and Frequency of Detection of Antibiotic Resistance Genes in Soil and on Vegetables at Harvest

Consumption of vegetables represents a route of direct human exposure to bacteria found in soil. The present study evaluated the complement of bacteria resistant to various antibiotics on vegetables often eaten raw (tomato, cucumber, pepper, carrot, radish, lettuce) and how this might vary with growth in soil fertilized inorganically or with dairy or swine manure. Vegetables were sown into field plots immediately following fertilization and harvested when of marketable quality. Vegetable and soil samples were evaluated for viable antibiotic-resistant bacteria by plate count on Chromocult medium supplemented with antibiotics at clinical breakpoint concentrations. DNA was extracted from soil and vegetables and evaluated by PCR for the presence of 46 gene targets associated with plasmid incompatibility groups, integrons, or antibiotic resistance genes. Soil receiving manure was enriched in antibiotic-resistant bacteria and various antibiotic resistance determinants. There was no coherent corresponding increase in the abundance of antibiotic-resistant bacteria enumerated from any vegetable grown in manure-fertilized soil. Numerous antibiotic resistance determinants were detected in DNA extracted from vegetables grown in unmanured soil. A smaller number of determinants were additionally detected on vegetables grown only in manured and not in unmanured soil. Overall, consumption of raw vegetables represents a route of human exposure to antibiotic-resistant bacteria and resistance determinants naturally present in soil. However, the detection of some determinants on vegetables grown only in freshly manured soil reinforces the advisability of pretreating manure through composting or other stabilization processes or mandating offset times between manuring and harvesting vegetables for human consumption.     

Plant community establishment in a restored wetland: Effects of soil removal

Question: This study investigated the establishment of wetland plant assemblages following soil removal and restored hydrology in a former agricultural field. The following questions were posed. Does plant community composition differ as a result of soil removal? Does soil removal reduce the frequency of non-wetland plants? Does soil removal reduce the frequency of non-native invasive plants? Location: The Panzner Wetland Wildlife Reserve (PWWR) in Summit County, northeastern Ohio, USA. Methods: During 2000–2001, restoration was conducted on two adjoining fields (3.9 ha total) by excavating the upper 40–50 cm of soil layer and establishing 12 10 m × 10 m undisturbed control plots. Preliminary data included seed bank composition and soil organic matter, estimated from three different soil depths on the control plots. In spring 2004, a 10 m × 10 m soil-removed plot was established adjacent to each control plot. Plant percent cover of all species was estimated within the center 5 m × 5 m of every plot. Above-ground biomass of all species from three 0.25-m² quadrats was collected. Environmental water measurements included water depth, temperature, dissolved oxygen, pH, and conductivity. Results: The top 10 cm of soil contained the most seeds, the highest species diversity, the greatest proportion of annual to perennial plants, and the lowest organic content. Obligate and facultative wetland plants were found in soil-removed plots while facultative upland and upland plants were found in control plots. The only plots with arable weeds were the control plots. However, plant communities on soil-removed plots in the North field, which had a higher elevation (ca. 15–20 cm), had a different species composition than soil-removed plots in the South field. Conclusions: The results of a controlled, replicated large-scale study on the effects of soil removal showed that soil removal altered both the biotic and abiotic environment, but that the proximity to the water table was the primary controlling factor in the assembly of plant communities.     

鼎湖山退化马尾松林、混交林和季风常绿阔叶林土壤全磷和有效磷的比较

土壤全磷和有效磷浓度的变化随林型和季节不同而异,总的来说,其大小顺序为:季风常绿阔叶林> 混交林>马尾松林(林型);夏季>冬季>春季>秋季(季节),有效磷浓度为:秋季>春季>冬季>夏季(季 节)。收割林下层和凋落物这种人为干扰活动对土壤全磷含量的影响不明显,但对土壤有效磷含量具有显著 的影响。在试验开始时(1990年5月),土壤全磷和有效磷浓度在马尾松林保护样地(停止人为干扰)和处理样 地(按当地习惯继续收割林下层和凋落物)间的差异均不显著。经七年多的试验后,土壤全磷浓度在保护样地 和处理样地间仍十分相似,但土壤有效磷浓度在保护样地显著高于处理样地,说明保护样地在停止人为干扰 后相对于继续受干扰的处理样地其林地条件得到了改善,从而使土壤有效磷含量也得到提高。只要停止人为 干扰,鼎湖山退化马尾松林土壤有效磷供应力是可以自然恢复到季风常绿阔叶林的水平。     

Monitoring the Spread of Recombinant DNA from Field Plots with Transgenic Sugar Beet Plants by PCR and Natural Transformation of Pseudomonas Stutzeri

Previous studies had shown that recombinant DNA can be detected for several months in soil after the deposition of litter from transgenic (tg) plants. Here we show by PCR monitoring of field releases of tg sugar beet plants that during the growth of the plants the soil close to the plants and also plant material contains recombinant DNA, in the form of extracellular molecules. Surprisingly, the monitoring also revealed the presence of tg DNA in many field plots (30–70%) in which tg plants were never grown. These studies and the further monitoring during other tg sugar beet release experiments by PCR and a novel bioassay (measuring the transforming potential of recombinant DNA for Pseudomonas stutzeri) indicated that recombinant DNA was only detectable in the surface soil of field plots and their vicinity where flowering of the tg beet plants was allowed. Recombinant DNA was found in soil at a distance of 50 m from pollen-producing plants surrounded by a strip with hemp plants as a containment regime. It is concluded that recombinant DNA is deposited in soil during the growth of tg sugar beets and that a major mechanism of recombinant DNA spread in the environment is the dispersal of pollen which allows recombinant DNA to persist in the field plot for at least a year.     

湘南红壤丘陵区不同植被类型下土壤肥力特征

以自然植被恢复长期定位试验为基础,通过分析自然恢复31a后形成的6个植被类型区(樟树、枫树、梓树、白檵木、唐竹、白茅草)、2个同期种植的人工植被区(湿地松、板栗)以及相邻裸地区0—100 cm土层pH值、有机质及主要养分含量的变化,明确了湘南红壤丘陵区不同植被类型对土壤肥力的影响。结果表明:(1)白茅草和唐竹区的土壤pH值显著高于裸地区,但枫树和白檵木区的土壤酸化明显。(2)土壤有机质、活性有机质、全P、速效P等指标表现为乔木草本灌木,碱解N、全K、速效K表现为灌木乔木草本,全N表现为乔木灌木草本。(3)土壤综合肥力优劣为:枫树区梓树区白檵木区樟树区唐竹区白茅草区湿地松区板栗区裸地区,自然恢复植被比人工植被更有利于土壤肥力的提高。     

暖温带森林土壤微生物量、群落结构和活性对植物地下碳源的响应

该研究以典型的亚热带—温带过渡区森林为对象,采用野外过程监测和控制试验相结合的方法,利用磷脂脂肪酸和土壤胞外酶活性分别表征土壤微生物群落结构和活性,并结合微环境因子,重点探究土壤微生物生物量、群落结构和活性对植物地下碳输入的响应特征。结果表明：在观测周期内,处理均能显著降低三组年龄段林分的土壤微生物量碳,其变化幅度在－8.72％~－5.72％之间,其中在80年的林分中降幅最大,而在160年的林分中降幅最小;微生物量氮的变化规律与相应的微生物量碳的变化规律相似,但与对照相比其差异性均未达到显著性水平;另外,经壕沟处理2~4个月后,所有林分的土壤微生物量碳和氮与对照相比出现增加的现象。处理均能对三组年龄段林分的土壤微生物群落结构产生不同程度的影响,其中40年林分的土壤微生物群落对处理的响应程度要高于另外两个年龄段的林分;与对照相比,壕沟处理样方的腐生真菌的相对丰富度均下降明显,其中在40年和80年林分中的下降幅度达到显著水平,而细菌、放线菌和丛枝菌根真菌均无明显变化;壕沟处理样方的水解酶(β-葡萄糖苷酶和N-乙酰-葡萄糖苷酶)活性均显著下降,而氧化酶(酚氧化酶和过氧化物酶)活性的变化相对较小,除80年的林分外,其余林分均不显著。此外,处理均不能显著影响土壤的含水量和温度。该研究结果为初步阐明全球气候变化背景下森林土壤微生物结构及其功能的变化特征以及更加精确预测未来森林土壤碳的变化趋势提供了科学依据。     

Prediction of occurrence of vascular plants in deciduous forests of South Sweden by means of Ellenberg indicator values

Abstract. In this study we present a new method for predicting the occurrences of species using data from deciduous forests in South Sweden. Complete species lists of vascular plants were compiled from 101 stands and from representative sample plots inside the stands. Soil samples from each stand were collected for determination of pH and nitrogen mineralization. Presence-absence data for species were fitted to the values of four environmental variables - soil moisture, soil reaction (pH), soil nitrogen and light - by means of Linear (Multiple) Logistic Regression (LLR), and Gaussian (Multiple) Logistic Regression (GLR). First, these values were estimated by calculating the weighted averages of Ellenberg indicator values. Second, the estimates for reaction and nitrogen were substituted by the real measurements of pH and mineralized NH₄⁺, keeping the Ellenberg estimates for light and moisture. The models were validated by an independent test data set. In general, the models had high predictive abilities. GLR fitted the species occurrences better to the environmental variables than LLR, but had a lower accuracy of prediction of species occurrence in the stands. The use of soil measurements instead of Ellenberg indicator values did not improve the predictive abilities of the models. The environmental conditions in the stand test set were successfully estimated by using species data from the plots. When using the species lists of the stands instead of plot data, a slightly better predictive ability was obtained. The collection of plot data, however, is easier and less time-consuming. The accuracy of prediction differed considerably between species.     

The effects of quantity and duration of simulated pollutant nitrogen deposition on root-surface phosphatase activities in calcareous and acid grasslands: a bioassay approach

A field and laboratory based bioassay has been developed to investigate the effects of the quantity and duration of simulated pollutant nitrogen (N) deposition on root-surface phosphomonoesterase (PME) activities in calcareous and acid grasslands. Seedlings of Plantago lanceolata were transplanted to a calcareous grassland and Agrostis capillaris seedlings were grown in microcosms containing soil from an acid grassland that had received either 7 yr (long-term) N additions or 18 months (short-term) N and phosphorus (P) additions. The bioassay revealed that short-term N treatments had little effect on the enzyme activity, whereas long-term N additions significantly increased PME activity within 7 d of transplanting into the field plots. Root-surface PME activity of A. capillaris was significantly reduced in soil that received additions of P. In the plots receiving long-term additions of N, a strong relationship was observed between extractable soil ammonium and root-surface PME activity. Soil ammonium concentrations accounted for 67% of the variation in PME activity of P. lanceolata in the calcareous grassland, and 86% of the variation in PME activity of A. capillaris in the acid grassland. These results provide evidence that N deposition may have considerable effects on the demand and turnover of P in ecosystems that are approaching or have reached N saturation.     

Effects of ammonium-N on development and infectivity of the take-all fungus

Effects of applications of a mixture of ammonium sulphate and mono-ammonium phosphate and of ammonium nitrate on the incidence of take-all disease of wheat (caused by Gaeumannomyces graminis var. tritici) and on subsequent inoculum levels were studied in field and glasshouse experiments. In a field experiment in Western Australia, on a sandy soil at pH 5·4, nitrogen applications had no detectable effect on disease severity at anthesis, but ammonium sulphate treatment increased the number of propagules of the pathogen in the soil. In a pot experiment, in which seed was sown in the field experiment soils, disease was greater in soil from plots treated with ammonium sulphate and least in soil from the nil-nitrogen plots, reflecting the respective inoculum levels in the field plot. However, treatment of the soils of lower inoculum with ammonium sulphate and ammonium nitrate during this pot experiment decreased disease. A second pot experiment confirmed the effectiveness of ammonium sulphate and ammonium nitrate in reducing take-all at lower inoculum levels, and their ineffectiveness at higher inoculum levels.     

Nitrogen supply affects arbuscular mycorrhizal colonization of Artemisia vulgaris in a phosphate-polluted field site

Root colonization by arbuscular mycorrhizal fungi (AMF) was investigated in industrially polluted grassland characterized by exceptionally high phosphorus levels (up to 120 g kg(-1) soil). Along a pollution-induced nitrogen gradient, soil and tissue element concentrations of Artemisia vulgaris plants and their mycorrhizal status were determined. Additionally, we compared mycorrhization rates and above-ground biomass of A. vulgaris at N-fertilized and control plots in the N-poor area. Despite high soil and tissue P concentrations, plants from N-deficient plots, which were characterized by low tissue N concentrations and N : P ratios, were strongly colonized by AMF, whereas at a plot with comparable P levels, but higher soil and plant N concentrations and N : P ratios, mycorrhization rates were significantly lower. Correlation analyses revealed a negative relationship between percentage root colonization of A. vulgaris by AMF and both tissue N concentration and N : P ratio. Accordingly, in the fertilization experiment, control plants had higher mycorrhization rates than N-fertilized plants, whereas the species attained higher biomass at N-fertilized plots. The results suggest that N deficiency stimulates root colonization by AMF in this extraordinarily P-rich field site.     

洞庭湖湿地3个林龄杨树人工林叶与土壤碳氮磷生态化学计量特征

选取洞庭湖洲滩湿地挖沟抬垄造林的6林龄、9林龄和13林龄杨树人工纯林为研究对象,通过比较不同林龄杨树叶及沟垄土壤的C、N、P含量差异,研究湿地杨树人工林不同生长阶段养分元素的分配格局及生态化学计量学特征,揭示杨树种植对洞庭湖湿地生态系统的影响。结果显示,叶N、叶P以及C∶P和N∶P与林龄显著相关,但叶C和C∶N与林龄不相关。3个林龄杨树人工林叶N∶P均大于16,说明P是限制洞庭湖杨树生长发育的主要因子,9林龄叶P量显著低于6林龄和13林龄,而N∶P和C∶P则显著高于6林龄和13林龄,说明P的限制在9林龄尤为显著。3个林龄湿地杨树人工林树垄和树沟土壤有机C、全N和C∶N呈现出与林龄和土层深度的负相关关系,但全P与两者没有显著关系。C∶P在树垄样地中呈现出与林龄和土层深度的负相关关系,而在树沟样地中呈现出与土层深度的正相关关系,与林龄无显著关系。N∶P在9林龄和13林龄树垄样地和6林龄树沟样地中与土层深度呈负相关关系,说明挖沟抬垄造林方式不利于土壤有机C和全N的积累,也不利于维持洞庭湖湿地土壤的肥力。     

Seasonal variation in organic and inorganic phosphorus fractions of temperate-climate sandy soils

Soils from an arable plot, a grassland plot and pasture plot were sampled over an 18-month period. Inorganic (P_i) and organic (P_o) soil phosphorus fractions were extracted sequentially with resin, NaHCO₃, and NaOH. Soil solution was sampled on the arable plot and pasture plot during 12 months with teflon suction cups, and the contents of P_i and P_o were determined.The patterns of the variation for all soil fractions were similar for the three plots. All soil P_i fractions were at minimum in the cool moist winter period. The soil P_o fractions varied less systematically than P_i fractions. The sum of P_o fractions had a winter maximum and a spring minimum. For all soil P fractions temporal variation was highly significant (p<0.0001). The magnitude of change in P_i and P_o soil fractions was 4–40 times greater than what would be expected from the magnitude of new N mineralization.The content of P in the inorganic soil P fractions was negatively correlated with soil moisture. The variation in organic soil P could not be explained by any single factor, but it is suggested that the variation is caused by changes in solubility rather than by biological transformations. Thus, physicochemical processes masked the impact of biological transformations on the temporal variation of soil phosphorus fractions.Both soil solution P_i and P_o varied significantly with time on field scale. In contrast to soil P_i fractions, solution P_i was initially low in the early autumn, increased by a factor 4 during the following 6 weeks, and thereafter decreased to a low level by the end of the sampling period. Soil solution P_o had several fluctuations during the sampling period.     

Bryophyte biomass and species richness on the Park Grass Experiment,Rothamsted, UK

The relationships between bryophyte biomass and species richness and soil pH, nutrient applications and vascular plant biomass and species richness were analyzed for the Park Grass Experiment (Rothamsted, UK). The study examined the abundance of bryophytes in relation to long-term fertilizer and lime application and to fertilizer treatments recently being ceased on some plots. The probability of bryophytes being present on a plot increased with increasing soil pH, and on plots at soil pH 3.3–4.5, the lowest values in this experiment, there were virtually no mosses present. Total bryophyte biomass decreased with increasing vascular plant biomass and vascular plant richness. Both bryophyte biomass and species richness showed a curvilinear response to soil pH. Bryophyte biomass was markedly increased on plots where nitrogen (N) fertilization had recently been ceased. The abundance of the common bryophyte species showed individualistic responses to treatments. N had a negative effect on the abundance of Brachythecium rutabulum. Increasing soil pH, and the application of phosphorus (P) and potassium (K) fertilizer together, had a positive effect on Eurhynchium praelongum. This species was also negatively affected by N, but tolerated larger amounts of it (100–150 kg ha^–1 N) than B. rutabulum. An ephemeral moss, Bryum subapiculatum, had a unimodal response to soil pH but showed no response to N, P, K or other explanatory variables.     

Growth and transpiration of maize and winter wheat in response to water deficits in pots and plots

Pots used for experiments conducted on plants grown in them create rooting environments that are affected by limited soil volume, which can affect various physiological processes, including transpiration, and plant growth. However, the applicability of results from pot experiments to the field has received limited attention. The objective of this study was to compare the growth and transpiration of maize (Zea mays L.) and winter wheat (Triticum aestivum L.) when grown in pots and field plots under various constant water deficits. The experiments were conducted under similar environmental conditions for both pots and plots. Transpirational responses at both transient (RTTr) and daily (RDTr) time scales to a decreasing fraction of available soil water (FASW) were analyzed. For a comparable FASW, there was a significant reduction in shoot dry weight and total transpiration for plants in pots compared to those in plots. A parabolic relationship between shoot dry weight and total transpiration existed and was not influenced by soil volume or crop type. The plot experiment data for both crops was consistent with pot data for the response of RDTr and RTTr to changes in FASW, which was represented by a linear-plateau function. However, the threshold values were significantly different for the two time scales. The threshold values and slopes of the linear-plateau function for maize and wheat were not significantly different in the response of RTTr to FASW, but were significantly different in the response of RDTr to FASW. Therefore, the transpirational responses of the selected maize and winter wheat hybrids to soil drought were different at the daily and transient time scales.     

中国农田土壤动物长期监测样地科学调查监测的实施方法

我国农田土壤动物面临严峻的多样性丧失问题, 建设监测样地并开展长期监测是解决该问题的重要途径, 但至今国内外仍缺乏农田土壤动物长期监测样地科学调查监测的实施方法。依据BCI 50 ha大型固定样地建设规范, 参照我国已建成的森林和农田土壤动物大型固定样地监测经验, 本文提出了农田土壤动物长期监测样地科学调查监测的实施方法。首先, 需要明确科学问题, 确定科学调查监测应遵守的基本原则。其次, 需要规范长期调查监测涉及的专业术语, 依据研究目的和实际情况选择地点和样地, 参照建设规范和农田特征建立农田土壤动物大型固定样地。第三, 以研究农田土壤动物多样性为核心, 揭示土壤动物在农田生态系统健康和功能中的作用, 有选择性地开展4类27项科学指标的长期监测工作, 要求按照统一的、规范化的工作流程开展野外调查和室内实验。最后, 要科学规范地完成标本的鉴定描述和保存保管, 研发体现农田土壤动物特征的数据库和管理信息系统。希望本文的研究结果能推动我国乃至世界范围的规范化样地建设和标准化网络监测, 为我国农田土壤动物评估与保护提供长期可靠的数据支撑。     

Downhill movement of litter and its implication for ecological studies in three types of forest in Japan

The amount of litter moving down the slope was measured in three types of forest, together with an examination of rain as a factor in bringing this about. The three forest types were a natural mixed stand ofPinus densiflora and hardwood trees (plot A), aCryptomeria japonica plantation (plot S) and aChamaecyparis obtusa plantation (plot H). The amount of moved litter was quite large in plots A and H, but relatively small in plot S. The rain factor had little influence on litter movement in plot A, but was the main cause of movement in plot S and (especially) plot H. It is suggested that measurement of litter input and output not only by traps above ground level, but also by ones on the ground is essential for determining the cycling of elements inC. obtusa forests. It is also suggested that the decomposition of leaf litter should be studied both on the soil surface and in the soil inC. obtusa forests.     

不同植被类型下红壤pH和交换性酸的剖面特征

研究湘南红壤丘陵区11种植被类型下施肥区域和未施肥区域红壤剖面(0～100 cm)pH及交换性酸的变化特征.结果表明: 施肥区域0～60 cm土层土壤的pH大小顺序为茶园<花生地<柑橘园,交换性酸含量大小为花生地≤柑橘园<茶园;种植茶树和花生后,表层(0～40 cm)相对底层(60～100 cm)均产生酸化,pH分别降低0.55和0.17,而种植柑橘后,土层间无显著差异.未施肥区域中,植被恢复区0～40 cm土层pH大小为白檵木林≤湿地松林<板栗园<白茅草地,交换性酸含量大小为白茅草地<板栗园<白檵木林≤湿地松林;天然林区0～20 cm土层中次生林和油茶林的pH均显著低于马尾松林0.34和0.20个单位,马尾松林和次生林交换性酸含量显著低于油茶林.与裸地相比,未施肥区域除白茅草地外,其他植被类型均加速了表层土壤酸化,其中天然次生林酸化最严重,pH降低0.52;未施肥区域除天然次生林外,其他植被类型均提高了深层土壤pH,其中白茅草地提升效果最显著,pH升高0.43.无论施肥区域还是未施肥区域,整体上随着土层深度的增加,植被类型或施肥对土壤酸度的影响越来越小.