Enzyme activities of aerobic lignocellulolytic bacteria isolated from wet tropical forest soils

Lignocellulolytic bacteria have promised to be a fruitful source of new enzymes for next-generation lignocellulosic biofuel production. Puerto Rican tropical forest soils were targeted because the resident microbes decompose biomass quickly and to near-completion. Isolates were initially screened based on growth on cellulose or lignin in minimal media. 75 Isolates were further tested for the following lignocellulolytic enzyme activities: phenol oxidase, peroxidase, β-d-glucosidase, cellobiohydrolase, β-xylopyranosidase, chitinase, CMCase, and xylanase. Cellulose-derived isolates possessed elevated β-d-glucosidase, CMCase, and cellobiohydrolase activity but depressed phenol oxidase and peroxidase activity, while the contrary was true of lignin isolates, suggesting that these bacteria are specialized to subsist on cellulose or lignin. Cellobiohydrolase and phenol oxidase activity rates could classify lignin and cellulose isolates with 61% accuracy, which demonstrates the utility of model degradation assays. Based on 16S rRNA gene sequencing, all isolates belonged to phyla dominant in the Puerto Rican soils, Proteobacteria, Firmicutes, and Actinobacteria, suggesting that many dominant taxa are capable of the rapid lignocellulose degradation characteristic of these soils. The isolated genera Aquitalea, Bacillus, Burkholderia, Cupriavidus, Gordonia, and Paenibacillus represent rarely or never before studied lignolytic or cellulolytic species and were undetected by metagenomic analysis of the soils. The study revealed a relationship between phylogeny and lignocellulose-degrading potential, supported by Kruskal–Wallis statistics which showed that enzyme activities of cultivated phyla and genera were different enough to be considered representatives of distinct populations. This can better inform future experiments and enzyme discovery efforts.     

农田土壤水分预测模型的研究进展及应用

本文对国内外土壤湿度的监测,预报发展情况进行了回顾,总结了国内外土壤水分监测方法及其原理,介绍了国内外土壤湿度预测模型的研究进展及其应用情况,讨论了传统的土壤水分平衡方程统计模型法,从土壤水分运动方程出发的物理学模型法,利用气象要素与土壤水相关关系为基础的统计预报法、及新兴的人工神经元网络和遥感数据估测法的优缺点,并对土壤水分研究工作所面临的问题进行了必要的阐述。     

The Enhancement of Soil Fertility,Dry Matter Transport and Accumulation,Nitrogen Uptake and Yield in Rice via Green Manuring

Readily available chemical fertilizers have resulted in a decline in the use of organic manure (e.g., green manures), a traditionally sustainable source of nutrients. Based on this, we applied urea at the rate of 270 kg ha⁻¹ with and without green manure in order to assess nitrogen (N) productivity in a double rice cropping system in 2017. In particular, treatment combinations were as follows: winter fallow rice-rice (WF-R-R), milk vetch rice-rice (MV-R-R), oil-seed rape rice-rice (R-R-R) and potato crop rice-rice (P-R-R). Results revealed that green manure significantly (p ≤ 0.05) improved the soil chemical properties and net soil organic carbon content increased by an average 117.47%, total nitrogen (N) by 28.41%, available N by 26.64%, total phosphorus (P) by 37.77%, available P by 20.48% and available potassium (K) by 33.10% than WF-R-R, however pH was reduced by 3.30% across the seasons. Similarly, net dry matter accumulation rate enhanced in green manure applied treatments and ranked in order: P-R-R > R-R-R > MV-R-R > WF-R-R. Furthermore, the total leaf dry matter transport (t ha⁻¹ ) for the P-R-R in both seasons was significantly higher by an average 11.2%, 7.2% and 36 % than MV-R-R, R-R-R, and WF-R-R, respectively. In addition, net total nitrogen accumulation (kg ha⁻¹ ) was found higher in green manure applied plots compared to the control. Yield and yield attributed traits were observed maximum in green manure applied plots, with treatments ranking as follows: P-R-R > R-R-R > MV-R-R > WF-R-R. Thus, results obtained highlight ability of green manure to sustainably improve soil quality and rice yield.     

镉胁迫对紫花苜蓿幼苗生理特性和镉富集的影响

以"甘农三号"紫花苜蓿幼苗为材料,在水培条件下,探究了在10 d内不同浓度(0～2.0 mmol·L^-1)镉(Cd)胁迫对其根长、茎长、生物量、叶绿素和丙二醛(MDA)含量、超氧化物歧化酶(SOD)和过氧化物酶(POD)活性、Cd富集及其亚细胞分布的影响。结果表明:低浓度(0.125 mmol·L^-1) Cd能促进幼苗根和茎的生长,增加叶片叶绿素含量,较高浓度(0.5～2.0 mmol·L^-1) Cd显著抑制幼苗根和茎的生长,叶绿素及生物量显著降低; Cd胁迫使MDA含量显著增加,而SOD和POD活性显著增强,其中Cd胁迫浓度为0.5mmol·L^-1时,SOD和POD活性达到最大值,这可能是植物对环境胁迫的一种应激保护反应; Cd在各亚细胞组分中的含量依次为细胞壁>细胞质>线粒体>叶绿体,且均随Cd胁迫浓度的升高而增加。当Cd胁迫浓度为0.125 mmol·L^-1时,水培10 d的紫花苜蓿幼苗单株地上部对Cd的净化率最高可达0.214%,而整盆植株在单位体积内对Cd的净化率最高可达15.5%;当Cd胁迫浓度为2.0 mmol·L^-1时,紫花苜蓿幼苗地上部Cd含量达89.36μg·g-1。这些结果表明紫花苜蓿对Cd具有很强的富集能力,虽未达到Cd超富集植物的临界标准,但从植株生物量、耐Cd能力、富集Cd量及对Cd的净化率等方面综合考虑,紫花苜蓿在Cd污染土壤的植物修复中具备良好的应用价值。     

不同林地清理方式对杉木林土壤肥力的影响

研究了杉木林采伐迹地及采伐后的炼山迹地的土壤物理性质、养分含量、微生物数量和酶活性.结果表明,采伐迹地的非毛管孔隙比杉木林地增加23%,自然含水量和毛管持水量则下降2%;炼山迹地土壤容重比杉木林地增加10%,非毛管孔隙、自然含水量和毛管持水量分别下降61%、48%和26%.采伐迹地有机质、全N、全P和全K含量分别比杉木林地下降14%、14%、3%和22%,炼山迹地分别下降37%、37%、47%和7%.采伐迹地碱解N和有效K含量分别比杉木林地增加24%和31%,有效P含量比杉木林地下降1%;炼山迹地的碱解N、有效P和有效K含量分别比杉木林地下降2%、43%和40%.采伐迹地的细菌、真菌和放线菌数量比杉木林地增加1.4、11.3和0.8倍;炼山迹地细菌数量比杉木林地减少24%,真菌和放线菌数量增加了.0和0.倍.采伐迹地脲酶、过氧化氢酶和纤维素分解酶活性分别为杉木林地1.9、1.6和2.1倍,而炼山迹地分别为后者的3.4%、90%和106%.湿润土壤有机质、全N和全P含量高,疏松多孔的土壤有利于碱解N、速效P、速效K积累和脲酶活性的增加.真菌数量随毛管孔隙的增加而减少.通气良好有利于提高土壤过氧化氢酶活性.     

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。     

水分亏缺对蚕豆光合特性影响的初步研究

本文报道了蚕豆现蕾至饱荚期不同时间土壤水分亏缺情况下的光合特性、光合产量及蚕豆水分亏缺敏感期。蚕豆现蕾后给予土壤干旱处理,光合速率、叶绿素含量、叶面积、气孔开度、生物产量及籽粒产量下降,但气孔密度和呼吸速率增加。水分亏缺使叶片光饱和点由50kLx降至30kLx,气孔开度日变化呈单峰(9—11时)曲线。始荚至盛荚期对土壤干旱最敏感,此期是蚕豆灌水的关键时期。     

Implications of biofuel policy‐driven land cover change for rainfall erosivity and soil erosion in the United States

Large‐scale conversion of traditional agricultural cropping systems to biofuel cropping systems is predicted to have significant impact on the hydrologic cycle. Changes in the hydrologic cycle lead to changes in rainfall and its erosive power, and consequently soil erosion that will have onsite impacts on soil quality and crop productivity, and offsite impacts on water quality and quantity. We examine regional change in rainfall erosivity and soil erosion resulting from biofuel policy‐induced land use/land cover (LULC) change. Regional climate is simulated under current and biofuel LULC scenarios for the period 1979–2004 using the Weather Research Forecast (WRF) model coupled to the NOAH land surface model. The magnitude of change in rainfall erosivity under the biofuel scenario is 1.5–3 times higher than the change in total annual rainfall. Over most of the conterminous United States (~56%), the magnitude of the change in erosivity is between ?2.5% and +2.5%. A decrease in erosivity of magnitude 2.5–10% is predicted over 23% of the area, whereas an increase of the same magnitude is predicted over 14% of the area. Corresponding to the changes in rainfall erosivity and crop cover, a decrease in soil loss is predicted over 60% of the area under the biofuel scenario. In Kansas and Oklahoma, the states in which a large fraction of land area is planted with switchgrass under the biofuel scenario, soil loss is estimated to decrease 12% relative to the baseline. This reduction in soil loss is due more to changes in the crop cover factor than changes in rainfall or rainfall erosivity. This indicates that the changes in LULC, due to future cellulosic biofuel feedstock production, can have significant implications for regional soil and water resources in the United States and we recommend detailed investigation of the trade‐offs between land use and management options.     

杉木人工林土壤活性有机质变化特征

在中国科学院会同森林生态实验站对第一代、第二代杉木林和地带性阔叶林土壤活性有机质主要组分进行了研究.结果表明,土壤活性有机质各组分含量均为杉木林低于阔叶林,而第二代杉木林又低于第一代杉木.第一代杉木林活性有机质总量、微生物生物量碳、水溶性有机碳和碳水化合物含量分别为18.79 g·kg^-1、421.7 mg·kg^-1、22.2 mg·kg^-1和136.3 mg·kg^-1,上述活性有机质组分在第二代杉木林中的含量分别是第一代杉木林的73.6%、87.9%、66.3%和3.2%,地带性阔叶林则分别为22.31 g·kg^-1、800. mg·kg^-1、361.1 mg·kg^-1和220.1 mg·kg^-1.相关性分析结果表明,土壤活性有机质各组分之间具有不同程度的相关性,其中土壤微生物生物量碳与其它活性有机质组分的相关性相对较高.     

Vascular plant 15N natural abundance in heath and forest tundra ecosystems is closely correlated with presence and type of mycorrhizal fungi in roots

In this study we show that the natural abundance of the nitrogen isotope 15, δ¹⁵N, of plants in heath tundra and at the tundra-forest ecocline is closely correlated with the presence and type of mycorrhizal association in the plant roots. A total of 56 vascular plant species, 7 moss species, 2 lichens and 6 species of fungi from four heath and forest tundra sites in Greenland, Siberia and Sweden were analysed for δ¹⁵N and N concentration. Roots of vascular plants were examined for mycorrhizal colonization, and the soil organic matter was analysed for δ¹⁵N, N concentration and soil inorganic, dissolved organic and microbial N. No arbuscular mycorrhizal (AM) colonizations were found although potential host plants were present in all sites. The dominant species were either ectomycorrhizal (ECM) or ericoid mycorrhizal (ERI). The δ¹⁵N of ECM or ERI plants was 3.5–7.7‰ lower than that of non-mycorrhizal (NON) species in three of the four sites. This corresponds to the results in our earlier study of mycorrhiza and plant δ¹⁵N which was limited to one heath and one fellfield in N Sweden. Hence, our data suggest that the δ¹⁵N pattern: NON/AM plants > ECM plants ≥ ERI plants is a general phenomenon in ecosystems with nutrient-deficient organogenic soils. In the fourth site, a␣birch forest with a lush herb/shrub understorey, the differences between functional groups were considerably smaller, and only the ERI species differed (by 1.1‰) from the NON species. Plants of all functional groups from this site had nearly twice the leaf N concentration as that found in the same species at the other three sites. It is likely that low inorganic N availability is a prerequisite for strong δ¹⁵N separation among functional groups. Both ECM roots and fruitbodies were ¹⁵N enriched compared to leaves which suggests that the difference in δ¹⁵N between plants with different kinds of mycorrhiza could be due to isotopic fractionation at the␣fungal-plant interface. However, differences in δ¹⁵N between soil N forms absorbed by the plants could also contribute to the wide differences in plant δ¹⁵N found in most heath and forest tundra ecosystems. We hypothesize that during microbial immobilization of soil ammonium the microbial N pool could become ¹⁵N-depleted and the remaining, plant-available soil ammonium ¹⁵N-enriched. The latter could be a main source of N for NON/AM plants which usually have high δ¹⁵N. In contrast, amino acids and other soil organic N compounds presumably are ¹⁵N-depleted, similar to plant litter, and ECM and ERI plants with high uptake of these N forms hence have low leaf δ¹⁵N. Further indications come from the δ¹⁵N of mosses and lichens which was similar to that of ECM plants. Tundra cryptogams (and ECM and ERI plants) have previously been shown to have higher uptake of amino acid than ammonium N; their low δ¹⁵N might therefore reflect the δ¹⁵N of free amino acids in the soil. The concentration of dissolved organic N was 3–16 times higher than that of inorganic N in the sites. Organic nitrogen could be an important N source for ECM and, in particular, ERI plants in heath and forest tundra ecosystems with low release rate of inorganic N from the soil organic matter. Received: 8 June 1997 / Accepted: 28 February 1998