流加氨水提高木聚糖酶活力初步研究

用正常产酶培养基和流加氨水产酶培养基培养Aspergillus niger J506,测定木聚糖酶的活性、酸性蛋白酶的活性和pH值。结果表明,用正常培养基培养时,木聚糖酶的活性在78~82 h达到产酶高峰,酶活力为226 U/mL。流加氨水培养,发酵液的pH值控制在4.0以上,木聚糖酶活力在86~90 h达到产酶高峰,活力为319 U/mL,比正常发酵提高了41.15%;而流加氨水条件下酸性蛋白酶活性从64 h开始比正常培养有明显降低。蛋白酶活力的降低和木聚糖酶活力的提高可能有一定关系。     

Liming Effects on Extractable Boron in Six Acidic Soils

A laboratory incubation study was conducted to study the influence of liming on extractable boron (B) in acidic soil. Six soils, three each from the Inceptisols and Alfisols, were incubated for 30 days with combinations of lime and B. The soils were acutely deficient in plant-available B (0.09–0.21 mg kg^?1). Only <50 percent of applied B was recovered from the soils in available form. Such recovery was lower in Alfisols than that in Inceptisols due to adsorption of a greater amount of added B with iron (Fe^?) and aluminium (Al^?) oxides in the former soil group. Required dose of lime showed an increase in availability of native soil B, particularly in Inceptisols (26 percent), and a net decrease in recovery of added B (32.5 percent) as compared to no lime control (41.6 percent). The results thus suggest that liming to acidic soils increases extractable B.     

Assessing the Feasibility of Olsen P and P Sorption Parameters in Acidic Soils

Plant-available phosphorus (P) and P adsorption capacities are important for crop growth in acidic soils. Olsen P test, which is based on extraction with bicarbonate for predicting the amount of soil P available to plants, was used in this work. Soil P-adsorption capacities were determined by Langmuir line equation. The purpose of this work was to examine the suitability of Olsen P for predicting phytoavailable P and P sorption parameters in acid soil. To this end, we (i) assessed the phytoavailable P by successively pot-cropping rice and (ii) P adsorption characteristics of soil and their relation with Olsen P. Plant-available P, estimated by Olsen P in tested soil, was correlated to labile P. Qm (phosphorus sorption maximum) was negatively correlated with K (P sorption strength). P buffering capacity of soils was P3 (the highest P rate) >P2 (the second highest P rate) >P1 (the lowest P rate) >P0 (no P adding) after 75 day’s rice growth, which indicated P replenishment capacity was different among P treatments. This also suggested that P of plant uptake may decrease soil buffering capacity, especially for soils that contained relatively lower amounts of P. Qm and K were not significantly correlated to Olsen P. Degree of P saturation and Olsen P shared the similar trend with the change of P application rates and sampling dates. We concluded P status in soil can be characterized by degree of P saturation and Olsen P in tested soil. They were able to explain P status from both agronomic and environmental aspects.

Abbreviations: Qm, P sorption maximum; K, P sorption strength; P3, highest P rate in soil; P2, second highest P rate in soil; P1, lowest P rate in soil; P0, P adding in soil.     

Chemical Fractions of Mn in Acidic Soils and Selection of Suitable Soil Extractants for Assessing Mn Availability to Maize (Zea Mays L.)

Twenty surface (0–15 cm) samples of acidic soils were analyzed for water soluble (WS), exchangeable (EX), lead displaceable (Pb-disp.), acid soluble (AS), manganese (Mn) oxide occluded (MnOX), organically bound (OB), amorphous Fe oxide occluded (AFeOX), crystalline iron (Fe) oxide occluded (CFeOX) and residual (RES) fractions of Mn, and also for extractable Mn in some common soil extractants: (diethylenetriaminepentaacetic acid (DTPA) (pH 7.3), DTPA (pH 5.3), AB-DTPA (pH 7.6), Mehlich-3 (pH 2.0), Modified Olsen, 0.005 M calcium chloride (CaCl₂), 1 M magnesium chloride (MgCl₂) and ion exchange resins. The WS-Mn fraction showed a significant and positive correlation with Mn extractable in DTPA (pH 5.3) and AB-DTPA (pH 7.6), while both WS-Mn and EX-Mn fractions correlated significantly and positively with Mn concentration and uptake by maize plants grown in these soils. The AB-DTPA (pH 7.6) and DTPA (pH 5.3) appeared suitable to assess the availability of Mn in acidic soils.     

Effects of chronically elevated nitrogen and sulfur deposition on sugar maple saplings: Nutrition,growth and physiology

At the Bear Brook Watershed in Maine (BBWM), we examined the effects of long-term experimentally elevated N and S deposition on foliar chemistry, growth, and photosynthetic capacity of sugar maple (Acer saccharum) saplings. The BBWM is a paired watershed system; one watershed has been acidified bimonthly with granular ammonium sulfate ((NH₄)₂SO₄) since 1989. The adjacent watershed is used as a reference. We observed a 56% increase in foliar Al and a 25% reduction in foliar Ca for sugar maple saplings on the treated watershed compared to reference. Foliar N (+15%), P (+10%), and K (+15%) were significantly elevated in treated saplings. Along with changes in foliar nutrients, there were significant differences in photosynthetic capacity.     

Colonization, ALP activity and plant growth promotion of native and exotic arbuscular mycorrhizal fungi at low pH

Soil acidity can affect arbuscular mucorrhizal fungi (AMF) in many aspects. In this study, by inoculating white clover (Trifolium ripens L.) with AMF at two pH levels (pH 5.0 and 6.0), we investigated the influences of low pH on the colonization, alkaline phosphatase (ALP) activity and promoting effect of AMF, and also compared the different responses of native AMF community and exotic species (Gigaspora margarita) to low pH. PCR-DGGE profiles revealed the obvious difference in native AMF community structure between low and high pH. Compared to low pH, high pH decreased the total and vesicle colonization, external hyphae length density of native AMF, but exerted no effect on those of exotic AMF. For both native and exotic AMF, high pH enhanced the proportions of arbuscule and fungal structure with ALP activity in colonized roots. Both native and exotic AMF promoted the shoot biomass, with greater increase at low pH than at high pH. Plant growth was more dependent on exotic AMF than on native AMF at both pH levels. The same trends were observed in P uptake as in biomass. Our study suggested that the increase in pH can exert inhibitory effects on AMF species native to acidic soil, including ecological (community structure), functional (ALP activity) and developmental (hyphal length, vesicle and arbuscule percentage, total colonization) aspects, but have no effect on exotic species in the present experiment.     

五氯酚在酸性土壤表面的吸附-解吸特征研究

本实验研究五氯酚在江西红壤和南京黄棕壤表面的吸附-解吸特征,结果表明:Freundlich和Langmuir等温吸附方程均能较好地描述PCP在两种土壤表面的吸附,且黄棕壤表面的最大吸附量大于红壤。用动力学方程对PCP在红壤中的吸附过程进行拟合,Elovich方程、双常数方程和一级动力学方程均得到较好的结果,其相关系数(R2)在0.96 ~ 0.99之间,达到极显著水平。Elovich方程反映出PCP在土壤表面吸附的能量非均质分布;而抛物线扩散方程不能描述PCP的吸附过程,其相关系数0.46 ~ 0.48。PCP在土壤中的解吸率与有机质含量和pH值相关,随有机质含量增加,PCP解吸率降低,即黄棕壤表土<黄棕壤底土,红壤表土<红壤底土;随模拟酸雨的pH值降低,土壤因对PCP的吸附能力增加,其解吸率降低。     

平衡施肥对芋头产量、品质和经济效益的影响

研究了平衡施肥对芋头产量、品质和经济效益的影响。试验结果表明,与CK（无肥处理）相比,不同施肥处理显著提高芋头产量达24．9％～76．7％,以增施钙肥处理（N3015K20Ca）增产效果最为显著;在N3015K20（OPT）的基础上配施钙、硼肥芋头产量分别增加15．1％和13．3％。不同施肥处理间芋头品质差异不显著。从2003—2007年,与CK相比,各施肥处理均可改善芋头品质（淀粉,氨基酸,粗蛋白,全P,全K）,且各项品质指标均呈逐年上升趋势。在处理OPT基础上配施钙、硼肥对芋头各品质指标无明显改善,甚至出现负效应。N30P15K20Ca和N30P15K20B处理的施肥利润最高。综合产量、品质和经济效益来看,N30P15K20Ca为芋头优质高产最佳养分组合。     

Quantification of ammonia-oxidising bacteria in limed and non-limed acidic coniferous forest soil using real-time PCR

Ammonia-oxidising bacteria (AOB) in limed and non-limed acidic coniferous forest soil were investigated using real-time PCR. Two sites in southern Sweden were studied, 244 Åled and Oxafällan. The primers and probe used earlier appeared to be specific to the 16S rRNA gene of AOB belonging to the β-subgroup of the Proteobacteria [Appl. Environ. Microbiol. 67 (2001) 972]. Plots treated with two different doses of lime, 3 or 6 t ha⁻¹, were compared with non-limed control plots on two occasions during a single growing season. Three different soil depths were analysed to elucidate possible differences in the density of their AOB communities. The only clear effect of liming on the AOB was recorded in the beginning of the growing season at 244 Åled. In samples taken in April from this site, the numbers of AOB were higher in the limed plots than in the control plots. At the end of the growing season the AOB communities were all of a similar size in the different plots at both sites, irrespective of liming. The number of AOB, determined using real-time PCR, ranged between 6×10⁶ and 1×10⁹ cells g⁻¹ soil (dw) at the two sites, and generally decreased with increasing soil depth. The results showed no correlation between community density and potential nitrification. This may indicate a partly inactive AOB community. Furthermore, more than 10⁷ cells g⁻¹ soil (dw) were recorded using real-time PCR in the control plot at 244 Åled, although Bäckman et al. [Soil Biol. Biochem. 35 (2003) 1337] detected no AOB like sequences in the same plots using PCR followed by DGGE. Taken together our results strongly suggest that the primers and probe set used are not well suited for quantifying AOB in acidic forest soils, which is probably due to an insufficient specificity. This shows that it is extremely important to re-evaluate any primers and probe set when used in a new environment. Consideration should be given to the specificity and sensitivity, both empirically and using bioinformatic tools.     

Effect of phosphate rock, lime and cellulose on soil microbial biomass in acidic forest soil and its significance in carbon cycling

Phosphate rock (PR), limestone, coal combustion by-product (CCBP) high in Ca and high organic manures are potential amendments for increasing agricultural production in the acidic soils of the Appalachian region. The objective of this study was to examine effects of PR, CCBP and cellulose addition on soil microbial biomass in an acidic soil based on the measurement of soil microbial biomass P (P _mic) and on the mineralization of organic matter. Application of PR alone or in combination with CCBP increased P _mic. The P _mic was far less when the soil received PR in combination with limestone than with PR application alone or PR in combination with CCBP. Either CCBP or limestone application alone considerably decreased P _mic in the soil due to reduced P solubility. Cellulose addition alone did not increase P _mic, but P _mic was significantly increased when the soil was amended with cellulose in combination with PR. The decomposition of added cellulose was very slow in the soil without PR amendment. However, mineralization of both native organic matter and added cellulose was enhanced by PR application. Mineralization of organic matter was less when the soil was amended with PR in combination with high rates of CCBP (> 2.5%) because PR dissolution varied inversely with amount of CCBP addition. Overall, CCBP had no detrimental effect on soil microbial biomass at low application rates, although, like limestone, CCBP at a high rate may decrease P _mic in P-deficient soils through its influence on increased soil pH and decreased P bioavailability in the soil. Application of PR to an acidic soil considerably enhanced the microbial activity, thereby promoting the cycling of carbon and other nutrients. Received: 11 December 1995