希拉穆仁草原不同放牧强度对植被群落特征和土壤团聚体的影响

[目的] 为探究草原不同放牧强度下植被群落的改变,解析群落特征变化对土壤团聚体的影响。[方法] 以希拉穆仁荒漠草原控制放牧试验区为研究对象,采用野外调查、室内分析相结合的方法,分析轻度放牧(LG)、中度放牧(MG)、重度放牧(HG)和禁牧(CK)下植被群落特征和土壤团聚体特征及二者的关系,揭示植物群落变化对土壤团聚体的影响。[结果] (1)植物群落物种数随放牧强度的增加而增加,LG的群落Shannon-Wiener多样性指数(H'')和Simpson优势度指数(D)显著低于其他放牧强度(p＜0.05)。地上生物量随放牧强度的增加而降低,HG的地上生物量显著低于其他放牧强度(p＜0.05)。不同放牧强度下地下生物量差异显著,且不同土层的地下生物量均以LG最高。(2)平均重量直径(MWD)和几何平均直径(GMD)的变化趋势与大团聚体含量一致,在0—5, 5—10 cm土层表现为随放牧强度的增加先增加后降低再增加(LG最高、MG最低)。(3)群落Shannon-Wiener多样性指数(H'')、Pielous均匀度指数(J'')、地上生物量、容重是影响大团聚体含量、MWD和GMD的显著性因子(p＜0.05)。[结论] 放牧强度对土壤团聚体稳定性具有负反馈调节作用,主要通过影响植被群落多样性指数(H''和J'')、地上生物量、土壤容重的变化而引起土壤团聚体稳定性的变化。该结果为希拉穆仁草原放牧强度选择及生态恢复工作提供理论支撑和科学依据。     

Development of specific PCR primers for identification and detection of <Emphasis Type="Italic">Phytophthora capsici</Emphasis> Leon

A PCR-based method was developed for the identification and detection of Phytophthora capsici in pepper plants. Three PCR primers (CAPFW, CAPRV1 and CAPRV2) specific for P. capsiciwere designed based on the sequence of its internal transcribed spacer regions. CAPFW/CAPRV1 amplify a 452 bp product from P. capsici DNA whereas CAPFW/CAPRV2 a 595 bp fragment; neither set amplifies DNA from pepper or several fungi pathogenic to pepper. In conventional (single-round) PCR, the limit of detection was 5 pg DNA for both primer sets, whereas in nested PCR the detection limit for both was of 0.5 fg. However, when the dilution series of target DNA were spiked with plant DNA, amplification declined two-fold in both conventional and nested PCR. The CAPFW/CAPRV2 set in conventional PCR was used to detect P. capsici DNA in inoculated plants. Detection occurred as soon as 8h post-inoculation in stem samples from infected but still symptomless plants. The method was also tested to detect fungal DNA in infected soils.     

连作障碍发生机制研究进展

目的研究不同前作对土壤生物化学性质的影响。方法利用化学和酶学分析及16S多样性测序技术,分析种植7年的不同前作[荞麦(FB)、油菜(FR)、小麦(FW)和绿肥(FG)]烟田土壤的养分、酶活性及细菌群落结构组成。结果(1) FR烟田土壤的有机质、全氮、碱解氮和有效磷含量最高,分别为30.04 g/kg、1.62 g/kg、143.50 mg/kg和88.09 mg/kg,FG烟田次之,但FG烟田速效钾的含量最高(240.10 mg/kg);FG烟田土壤蛋白酶和磷酸酶的活性最高,分别为709.02 μg/(g·d)(酪氨酸)和306.60 μg/(g·h)(对硝基酚),而其脲酶和蔗糖酶的活性仅低于FW烟田,且无显著性差异(P>0.05)。(2)在细菌群落组成上,FB、FG、FW和FR烟田分别检测出770、670、654和597属,归属于Actinobacteria、Proteobacteria、Chloroflexi和Acidobacteria等36门,其中Actionbacteria和Proteobacteria相对丰度最高,分别为26.87%~45.21%和25.82%~30.69%,Treptomyces、Bradyrhizobium、Bacillus和Mycobacterium等拮抗菌和Bradyrhizobium、Rhizobium和Paenibacillus等固氮菌在FB烟田土壤细菌群落的相对丰度最高。结论不同前作对烟田土壤理化性质、酶活性和细菌群落结构的影响不同,绿肥提高了土壤有机质和养分含量以及酶活性;而荞麦改善和提高了烟田土壤细菌种群结构和多样性。     

玉米根系分泌物对烟草黑胫病菌的抑制活性及其抑菌物质分析

目的明确玉米、辣椒单作和间作种植后根围土壤细菌群落的变化与病害发生的关系,解析土壤微生物在玉米和辣椒多样性种植中控制病害的作用。方法比较玉米/辣椒间作和分别单作后根围土壤微生物对玉米小斑病和辣椒疫病发生的影响,并应用Illumina Miseq高通量测序技术比较不同处理根围细菌群落的差异。结果单作玉米的根围土壤微生物能显著抑制辣椒疫病的发生(P<0.05),辣椒单作、玉米/辣椒间作后玉米根围土壤微生物降低玉米小斑病的趋势明显。根围土壤细菌群落分析结果表明：单作玉米根围气单胞菌属、堆囊菌属和固氮螺菌属等的相对丰度显著高于间作玉米和单作辣椒根围(P<0.05);单作辣椒和间作玉米根围土壤中拟杆菌门相对丰度上调,并且其中的拟杆菌属、农研丝杆菌属、鞘氨醇杆菌属和Muribaculum的相对丰度也显著上调(P<0.05)。结论玉米/辣椒间作和间作后有利于帮助彼此降低病害的发生。单作或间作后导致土壤细菌群落的变化是其缓解病害发生的重要机制。     

施肥对热带雨林下种植砂仁土壤氮矿化和硝化作用的影响

采用封顶埋管法(Close-TopIncubation)研究了施肥后西双版纳热带雨林下种植砂仁土壤的氮素净氨化、净硝化和净矿化速率。结果表明,种植砂仁的热带雨林土壤有机氮的净氨化、硝化和矿化速率明显受外来无机氮的影响,施入铵态氮肥后,土壤中的氨化速率明显提高(P<0.01),由对照土壤的-0.66(mg·kg-1·30d-1)增加至施肥处理土壤的1.65(mg·kg-1·30d-1),但硝化速率和矿化速率却显著降低(P<0.01),分别由对照土壤的6.79(mg·kg-1·30d-1)和6.13(mg·kg-1·30d-1)减少至施肥处理土壤的2.60(mg·kg-1·30d-1)和4.25(mg·kg-1·30d-1),导致了土壤中NH4+-N的积累。     

Comparison of uptake of different N forms by soil microorganisms and two wet-grassland plants: A pot study

Two common plant species of temperate wet grasslands, Carex acuta and Glyceria maxima, were tested for their preferences in the uptake of different nitrogen (N) sources (amino acid, ammonium, nitrate) and their ability to compete for these sources with soil microorganisms. The experiment was a one-day incubation study with plants growing in soil obtained from the field, which was supplied with a solution containing the three N sources, one at a time labeled with ¹⁵N. The bulk of the N demand of both species was covered by nitrate-N, which was the dominant N form in the soil at the time of the experiment. Ammonium-N was taken up less strongly, and organic N formed only a negligible part of their nutrition. The assimilated inorganic N was preferentially transported to apical meristem of the youngest leaf, while organic N remained mostly in the roots. The fast-growing Glyceria took up more N and was a better competitor vis-à-vis soil microbes for rarer N forms than Carex. However, both plants were poor competitors for N vis-à-vis soil microbes, irrespective of the N form. Microbes took up nitrate ca. five times faster and organic N more than a hundred times faster than plants. Correspondingly, the calculated turnover time of microbial N was 17 days, compared to 40 days for N in plant roots. A significant amount of added ¹⁵N was found at non-exchangeable sites in the soil, which points to the importance of microbial N transformation and abiotic N fixation for N retention in soil. In summary, the preferential assimilation of inorganic N by the wetland plants studied here and their poor ability to compete for N with soil microbes over the short term agree with the results of studies carried out with other species from temperate grasslands.     

Greenhouse gas emissions in response to straw incorporation,water management and their interaction in a paddy field in subtropical central China

A field experiment was conducted to study the effects of combination of straw incorporation and water management on fluxes of CH₄, N₂O and soil heterotrophic respiration (Rh) in a paddy field in subtropical central China by using a static opaque chamber/gas chromatography method. Four treatments were set up: two rice straw incorporation rates at 0 (S1) and 6 (S2) t ha^?1 combined with two water managements of intermittent irrigation (W1, with mid-season drainage) and continuous flooding (W2, without mid-season drainage). The cumulative seasonal CH₄ emissions for the treatments of S1W2, S2W1 and S2W2 increased significantly by 1.84, 5.47 and 6.63 times, respectively, while seasonal N₂O emissions decreased by 0.67, 0.29 and 1.21 times, respectively, as compared to S1W1 treatment. The significant increase in the cumulative Rh for the treatments S1W1, S2W1 and S2W2 were 0.54, 1.35 and 0.52 times, respectively, in comparison with S1W2. On a seasonal basis, both the CO₂-equivalents (CO₂e) and yield-scaled CO₂e (GHGI) of CH₄ and N₂O emissions increased with straw incorporation and continuous flooding, following the order: S2W2>S2W1>S1W2>S1W1. Thus, the practices of in season straw incorporation should be discouraged, while mid-season drainage is recommended in paddy rice production from a point view of reducing greenhouse gas emissions.     

调亏灌溉和氮处理对小桐子生长及水分利用的影响

为了研究阶段水分亏缺(亏水+不亏水W_LW_H、不亏水+亏水W_HW_L、亏水+亏水W_LW_L、不亏水+不亏水W_HW_H)和不同施氮量(N_Z:0,N_L:0.2 g/kg,N_H:0.4 g/kg)对小桐子生长、生理指标和灌溉水利用效率的影响,通过盆栽试验,发现W_LW_H的生长和灌溉水利用效率均显著高于W_HW_L;作物的灌溉水利用效率随施氮量的增大而呈现先增大后减小的趋势,在N_L水平下达到最大值;与高水高氮的处理N_HW_HW_H相比,中水低氮处理N_LW_LW_H节约灌溉水27%,节约氮肥使用量50%,小桐子株高减少31%、总干物质量减少35%,灌溉水利用效率减少13%,但茎粗增加13%,根冠比增加20%.可见小桐子在第一阶段处理(40~90 d)幼树期对水分的需求量较小,适度的亏缺灌溉可提高灌溉水利用效率;小桐子在第二阶段处理(90~140 d)处于旺长期,对水分的需求量较大,增大灌水量可大幅度促进小桐子生长及其干物质量的积累.全生育期实施亏缺灌溉,可提高小桐子自身适应外界环境能力,抗干旱胁迫能力也逐渐增强,但W_LW_L水平下的小桐子生长缓慢.经综合分析,认为处理N_LW_LW_H可作为干旱地区条件下的小桐子灌溉和施氮制度.     

Pulverizing Soils for Laboratory Analysis

Soil-testing laboratories utilize a range of grinder types to pulverize soils for laboratory analysis. This study was conducted to evaluate the effects of soil particle diameter and laboratory subsample size on analysis variability on nitrate, Bray 1 extractable phosphorus (P), extractable potassium (K), and soil organic matter (SOM). Four soils collected for the Agricultural Laboratory Proficiency Program were pulverized using four types of commercial grinders and analyzed for particle-size distribution, P, and K. In a second study, soils were pulverized to pass sieves of 2.0, 1.0, and 0.50 mm and subsampled for P, K, and SOM. Results of the commercial grinders indicate a range in mean particle diameters from 0.15 to 0.60 mm, with the lowest for the grinder utilizing a hammer mill design. Sieve-size analysis results indicate that the coarsest 2.0-mm fraction had the largest variability for all soil analyses evaluated. Analyte variability decreased with decreasing sieve size. Mean Bray P, K, and SOM-LOI (Loss-on-Ignition) mean concentrations were not statistically significantly different across the sieve sizes evaluated. Laboratory analysis variability for extractable Bray P increased as subsample size was reduced.     

江西水土流失对防洪的影响及防治对策

江西省水土流失面积 3 5 2万km2 ,严重破坏了生态环境。水土流失导致河床和水库淤积 ,加剧了洪涝灾害程度。鄱阳湖承担着长江巨大超额洪水的调蓄 ,但湖区面积已由 2 0世纪 5 0年代初期的 5 10 0多km2 萎缩到现在的 3 95 0多km2 ,容积缩小了 72亿m3。本省境内的“五河”流入鄱阳湖内的水量达 14 0 0多亿m3,是该湖容积的 4倍多 ,可见搞好水土保持对长江防洪的重要意义。水土保持措施已在防洪减灾中发挥了重大作用 ,应把水土保持生态环境建设作为长江和本省新世纪水利发展战略的重要内容