广西木论喀斯特森林土壤养分水平与植被及地形的关系

研究了广西木论喀斯特森林原生植被和次生植被的土壤养分特征,测定了陡坡、缓坡、洼地3种主要地形内林地0～5 cm表层土壤中的有机质(SOM)、氮、磷、钾含量,以及它们在石土面、土面两类主要小生境间的差异.结果表明:林分成熟度高、优势种不明显的原生林积累了高水平的SOM,缓坡石土面最高,达345 g kg-1,洼地的含量较低,但仍在80 g kg-1以上;土壤全氮(TN)、碱解氮(AN)含量也较高.以红背山麻杆(Alchornea trewioides)、广西野桐(Mallotus conspuyrcatus)、伞花木(Eurycorymbus cavderiei)等为优势种的次生林,物种多样性较原生林低,SOM、TN、AN含量也低,缓坡石土面和土面小生境的SOM分别为110 g kg-1和77 g kg-1,是原生林的32%和35%,下降幅度最大,其次为陡坡,而洼地的差异不明显.全磷(TP)、有效磷(AP)、全钾(TK)、有效钾(AK)含量在两林型间差异无明显规律.原生林和次生林土壤养分含量(除TK外)以缓坡>陡坡>洼地;但次生林中三者间无显著差异.同类型样地内小生境土壤养分含量(除TK外)均为石土面含量高于土面.     

Bioleaching of heavy metals from contaminated soil using <Emphasis Type="Italic">Acidithiobacillus thiooxidans</Emphasis>: effect of sulfur/soil ratio

Bioleaching of heavy metals from contaminated soil was carried out using indigenous sulfur oxidizing bacterium Acidithiobacillus thiooxidans. Experiments were carried out by varying sulfur/soil ratio from 0.03 to 0.33 to evaluate the optimum ratio for efficient bioleaching of heavy metals from soil. The influence of sulfur/soil ratio on the bioleaching efficiency was assessed based on decrease in pH, increase in oxidation–reduction potential, sulfate production and solubilization of heavy metals from the soil. Decrease in pH, increase in oxidation–reduction potential and sulfate production was found to be better with the increase in sulfur/soil ratio. While the final pH of the system with different sulfur/soil ratio was in the range of 4.1–0.7, oxidation reduction potential varied from 230 to 629 mV; sulfate production was in the range of 2,786–8,872 mg/l. Solubilization of chromium, zinc, copper, lead and cadmium from the contaminated soil was in the range of 11–99%. Findings of the study will help to optimize the ratio of sulfur/soil to achieve effective bioleaching of heavy metals from contaminated soils.     

连作对三七种子萌发及种苗生长的影响

为进一步明确三七的连作效应,以不同种植年限及不同空间分布的土壤为栽培基质,研究了连作对三七种子萌发及种苗生长的影响。结果表明:连作使三七种子萌发的最大速度增加,种子的发芽势变化不大,而发芽率、发芽指数和快速发芽期则呈明显降低或变短的趋势;与根区外土相比,根区土和根区下土使三七种子的发芽势、发芽率和发芽指数显著降低,对种子萌发的最大速度也有降低的作用;种植1年三七的土壤(1年土)对后茬三七种苗的生长并无明显障碍效应,2年土比3年土具有更强的抑制三七种苗生长的作用。连作对三七种子萌发及种苗生长均会产生明显的障碍效应,自毒作用可能只是造成三七连作障碍的原因之一。     

Research progress on the effects of soil erosion on vegetation

The relationship between vegetation and soil erosion deserves attention due to its scientific importance and practical applications. A great deal of information is available about the mechanisms and benefits of vegetation in the control of soil erosion, but the effects of soil erosion on vegetation development and succession is poorly documented. Research shows that soil erosion is the most important driving force for the degradation of upland and mountain ecosystems. Soil erosion interferes with the process of plant community development and vegetation succession, commencing with seed formation and impacting throughout the whole growth phase and affecting seed availability, dispersal, germination and establishment, plant community structure and spatial distribution. There have been almost no studies on the effects of soil erosion on seed development and availability, of surface flows on seed movement and redistribution, and their influences on soil seed bank and on vegetation establishment and distribution. However, these effects may be the main cause of low vegetation cover in regions of high soil erosion activity and these issues need to be investigated. Moreover, soil erosion is not only a negative influence on vegetation succession and restoration, but also a driving force of plant adaptation and evolution. Consequently, we need to study the effects of soil erosion on ecological processes and on development and regulation of vegetation succession from the points of view of pedology and vegetation, plant and seed ecology, and to establish an integrated theory and technology for deriving practical solutions to soil erosion problems.     

Algae as Bio-fertilizers: Between current situation and future prospective

Bio-fertilization is a sustainable agricultural practice that includes using bio-fertilizers to increase soil nutrient content resulting in higher productivity. Soil micro-flora has been exposed to improve soil fertility and increase biomass productivity and identified as a correct environmentally friendly bio-based fertilizer for pollution-free agricultural applies. The majority of cyanobacteria can fix nitrogen from the atmosphere and several species including Anabaena sp., Nostoc sp., and Oscillatoria angustissima is known to be effective cyanobacterial based bio fertilizers. Acutodesmus dimorphus, Spirulina platensis Chlorella vulgaris, Scenedesmus dimorphus, Anabaena azolla, and Nostoc sp. are some of the green microalgae and cyanobacteria species that have been successfully used as bio fertilizers to boost crop growth. Also, Chlorella vulgaris is one of the most commonly used microalgae in bio fertilizer studies. The addition of seaweed species that are Sargassum sp. and Gracilaria verrucosa leads to chemical changes as a soil fertility indicator on clay and sandy soils, and the addition of seaweed conditioner to soil can improve its organic content, return pH to normal, and reduce C/N ratio in both sandy and clay soil. This review provides an effective approach to increase soil fertility via environmentally friendly bio-based fertilizer using micro and macro algae. Instead of the usage of inorganic and organic fertilizers that have polluted impacts to soil as aggregation of heavy metals, in addition to there their human carcinogenic effects.     

杉木人工林土壤微生物生物量碳氮特征及其与土壤养分的关系

研究了湖南会同红黄壤区杉木人工林和常绿阔叶林土壤微生物量和养分状况.结果表明,该区杉木人工林取代地带性常绿阔叶林和杉木连栽后,土壤微生物碳、氮和土壤养分含量下降,土壤严重退化.在0～10 cm土层内,常绿阔叶林土壤微生物碳和氮含量为800.5和84.5 mg·kg^-1,分别是第1代杉木林的1.90和1.03倍、第2代杉木林的2.16和1.27倍;在10～20 cm土层内,常绿阔叶林土壤微生物碳和氮含量为475.4和63.3 mg·kg^-1,分别是第1代杉木纯林的1.86、1.60倍和第2代杉木林的2.11和1.76倍.在0～10 cm 和10～20cm土层内,杉木人工林取代常绿阔叶林和杉木栽植代数增加后,土壤全氮、全钾、铵态氮和速效钾含量均明显降低,但差异并不显著.人工杉木林林分组成单一,其凋落物分解慢、归还养分数量少;炼山等造成的表土流失是杉木人工林土壤微生物量和养分库退化的重要原因.土壤微生物碳与土壤全氮、铵态氮、全钾和速效钾含量呈极显著的正相关,土壤微生物氮与土壤养分含量也达到极显著水平.     

甲氰菊酯和辛硫磷及其混剂的土壤微生物降解

The degradation rates of fenpropathrin, phoxim and their mixture in un-sterilized soil were much quicker-than those in sterilized soil, which indicated that soil microorganisms played a significant role in the degradation pro-cessin soil. The half-life (T0.5) in un-sterilized soil was 56.2 d for fenpropathrin, 57.8 d for mixed fen-propathrin, 48.2 d for phoxim, and 41.7 d for mixed phoxim. The corresponding half-life (T0.5) in sterilizedsoil was 135.1 d, 147.3 d, 123.6 d, and 126.2 d, respectively. There were no significant differences for degradation rates between single use and mixed use of fenpropathrin and nhoxirn.     

傅家边丘陵山地滨梅根围AM真菌与土壤酶活性的关系

为揭示AM真菌对宿主滨梅（Prunus maritima）的作用特点及对根部土壤酶活性的影响,于2009年4月、7月和10月分别从江苏傅家边丘陵山地滨梅根围分0～10、10～20、20～30、30～40、40～50 cm 5个土层采集土壤样品,观察滨梅AM菌根结构,测定了AM真菌侵染率、孢子密度、土壤磷酸酶、脲酶活性及有效磷、碱解氮含量,着重分析了AM真菌与土壤酶活性之间的关系。结果表明,滨梅能与AM真菌形成良好的共生关系,共生体为泡囊-丛枝结构;AM真菌侵染率和孢子密度分别在7月份和10月份最高,均出现在0～20 cm土层,并随土层加深而下降;AM真菌侵染率与土壤酸性磷酸酶、中性磷酸酶、碱磷酸酶活性显著正相关,而与脲酶活性无相关性;AM真菌孢子密度与碱性磷酸酶、脲酶活性呈极显著正相关关系;孢子密度与土壤有效磷、土壤碱解氮含量显著正相关,但AM真菌侵染率仅与土壤有效磷含量显著正相关;孢子密度与菌根侵染率之间无相关性。可见,滨梅AM真菌侵染率与孢子密度有明显的时空分布并与土壤因子尤其是某些土壤酶活性密切相关,且AM菌根的形成是滨梅适应丘陵山地干旱贫瘠环境的有效对策之一。     

Can soil Chytridiomycota survive and grow in different osmotic potentials?

Twenty isolates from soil in the orders Spizellomycetales, Blastocladiales and Chytridiales (Chytridiomycota) grew on complex solid media supplemented with 10 g l⁻¹ sodium chloride. In a synthetic liquid medium, 4.4 g l⁻¹ sodium chloride strongly inhibited growth in three of the five isolates, possibly because of the effect of the ions or osmolarity of the solution. The maximum concentration for growth in synthetic liquid medium with different osmotic potentials using polyethylene glycol (PEG) varied considerably amongst the isolates. Three patterns of growth with increasing concentrations of PEG were evident among isolates within the genus Rhizophydium. Up to the concentration where growth ceased, the dry weight of each isolate either decreased, remained constant, or in one case, increased. Most of the fungi survived when incubated at room temperature for 7 d in complex liquid media supplemented with 35 g l⁻¹ sodium chloride or 300 g l⁻¹ PEG. These data indicate that soil Chytridiomycota can survive various osmotic potentials that may occur during the wetting and drying phases in soils.