喀喇昆仑山盖孜河水文水资源特性分析

喀喇昆仑山河流自有水文资料记载以来 ,近 10年洪灾发生频率明显高于以往 ,人民的生命财产损失程度也大幅度增加。在分析了盖孜河流域的径流及气候多年变化过程后 ,认为洪灾频发的原因是近年来流域内降水及气温呈上升趋势 ,导致高山冰川退缩 ,河流径流增加 ,洪灾增大、频率增高 ;小区域多年气候变化过程从侧面印证了我国西北地区气候由暖干向暖湿变化。     

限水灌溉对转基因抗虫棉产量形成的影响

采取限水灌溉的方法,研究了灌水对棉花产量形成的影响。研究结果表明,合理灌水能促进棉花开花成铃,延长最佳成铃时段,增加棉株优质节位的成铃数,单株籽棉干物重增加23.4%～61.9%,产量提高16.8%～45.3%。灌水量以675m3/hm2效果最好,灌水效益高达0.57kg/m3,灌水量达1350m3/hm2增产幅度下降,灌水效益仅0.21kg/m3。     

Contrasting development of soil microbial community structure under no-tilled perennial and tilled cropping during early pedogenesis of a Mollisol

A range of agricultural practices influence soil microbial communities, such as tillage and organic C inputs, however such effects are largely unknown at the initial stage of soil formation. Using an eight-year field experiment established on exposed parent material (PM) of a Mollisol, our objectives were to: (1) to determine the effects of field management and soil depth on soil microbial community structure; (2) to elucidate shifts in microbial community structure in relation to PM, compared to an arable Mollisol (MO) without organic amendment; and (3) to identify the controlling factors of such changes in microbial community structure. The treatments included two no-tilled soils supporting perennial crops, and four tilled soils under the same cropping system, with or without chemical fertilization and crop residue amendment. Principal component (PC) analysis of phospholipid fatty acid (PLFA) profiles demonstrated that microbial community structures were affected by tillage and/or organic and inorganic inputs via PC1 and by land use and/or soil depth via PC2. All the field treatments were separated by PM into two groups via PC1, the tilled and the no-tilled soils, with the tilled soils more developed towards MO. The tilled soils were separated with respect to MO via PC1 associated with the differences in mineral fertilization and the quality of organic amendments, with the soils without organic amendment being more similar to MO. The separations via PC1 were principally driven by bacteria and associated with soil pH and soil C, N and P. The separations via PC2 were driven by fungi, actinomycetes and Gram (−) bacteria, and associated with soil bulk density. The separations via both PC1 and PC2 were associated with soil aggregate stability and exchangeable K, indicating the effects of weathering and soil aggregation. The results suggest that in spite of the importance of mineral fertilization and organic amendments, tillage and land-use type play a significant role in determining the nature of the development of associated soil microbial community structures at the initial stages of soil formation.     

Root zone temperature alters storage root formation and growth of sweetpotato

Large mounds amended with plant residues are a common cultivation method for sweetpotato (Ipomoea batatas) in the western parts of the Papua New Guinea highlands, with a suggested benefit of elevated root zone temperature (RZT) from decomposition. This study aimed to evaluate whether RZT affects the formation and growth of sweetpotato storage roots. Experiments evaluated the effects of a constant elevated RZT on the Beauregard cultivar and of a short‐term increase in RZT on the Beauregard and Northern Star cultivars. Plants were grown in 18‐L pots divided into a control compartment (constant RZT at 20°C) and a treated compartment (RZT at 30, 40 or 50°C). Constant elevated RZT was maintained until harvest, while short‐term increase in RZT occurred in weeks 2 and 3 only. Constant elevated RZT did not affect the total number of storage roots, but RZT of 30°C and above reduced the dry‐biomass of storage roots. The short‐term increase in RZT did not alter the total number or dry‐biomass of storage roots in Beauregard, while both of these attributes were reduced at RZT of 40°C or above in Northern Star. Elevated RZT inhibited dry‐biomass accumulation of storage root, with a more pronounced impact at constant elevated RZT. These results demonstrate that any benefits of the mound culture on sweetpotato yield production do not arise through the influence of temperature elevation.     

外源蔗糖对离体条件下换锦花小鳞茎发生的影响

从形态学、组织细胞学、生理生化水平、分子水平等多层面探究外源蔗糖浓度对换锦花（Lycoris sprengeri）离体小鳞茎发生的影响。结果表明，MS培养基中外源蔗糖缺失时，离体换锦花鳞茎无法产生小鳞茎，蔗糖浓度为30 或60 g ? L-1时小鳞茎正常发生，但对小鳞茎发生数量影响不大。鳞片内的蔗糖及可溶性糖含量在腋芽形成前不断积累，且鳞片基部淀粉粒的积累为此处小鳞茎的发生提供物质基础。蔗糖促进了茉莉酸甲酯（MeJA）在植物体内的积累，抑制了LsWIP1、LsERS2和LsEIN2基因表达量的异常上升，表明蔗糖可能作为信号分子启动了相关损伤保护机制，并促进了小鳞茎的发生。     

基于动态平衡视角下现代足球阵型演变的沿革与变迁

拟在动态平衡的视角下对现代足球阵型的演变历程进行梳理与整合，希望对阵型之间的关联及其对足球运动发展的影响提供见解，对阵型演变的不同阶段进行探讨，探寻足球攻守平衡与不同阵型的嬗变关系，同时也为推动未来足球阵型演变对战术打法的影响研究提供参考依据。采用文献资料、系统分析、专家访谈和逻辑分析等方法，对现有的足球阵型发展的概况进行分析之后，认为现代足球阵型的演变历程不断交替出现攻守的平衡与不平衡，正是交替出现的状况促进了阵型的改变，进而影响了阵型的发展。当阵型的发展过程中出现攻守平衡时，就有其它后来者对该阵型进行学习、模仿、改进、提高。当阵型的发展过程中出现攻守不平衡，攻强于守或者守强于攻时，就会促进阵型的演变向攻守平衡的方向发展，因此就会出现阵型的发展处于不平衡-平衡-不平衡-再到平衡的态势，从而形成比赛阵型发展本身的稳定与不稳定状态交替出现。研究认为，世界足球阵型演变的过程是一种动态的、不断发展的、维持某种平衡与稳定的、平衡和不平衡交替运动的情况，即动态平衡的状态。提出将现代足球阵型演变的过程分为不同的阶段，每一个阶段内，都分别出现攻守平衡与攻守不平衡的状态，而这种平衡与不平衡的存在与区别、斗争与转化正是足球阵型演变与发展的规律。     

Comparison of Salt and Drought‐Stress Effects on Maize Growth and Yield Formation with Regard to Acid Invertase Activity in the Kernels

The long‐term effects of salt stress (11 dS m^?1) and drought stress (35 % WHC) were investigated for two maize genotypes, focusing on the relation between metabolic changes around the time of pollination and the impact on yield determinants at maturity. The relatively salt‐resistant hybrid Pioneer 3906 and the relatively drought‐resistant hybrid Fabregas were compared. The experiments were conducted in large plastic containers in a vegetation hall in two consecutive years (2011 and 2012). Plant height and leaf area were significantly reduced under both stress conditions. The transpiration rate was only slightly reduced under drought stress; but under salt stress, a significant reduction occurred 40–53 days after sowing. As a significant increase in sucrose concentrations was observed in the salt‐treated maize kernels 2 days after pollination, the availability of assimilates was not limiting and the plants could afford to save water by reduced stomatal opening. Although under both stress conditions the soluble acid invertase activity was reduced 2 days after pollination, concomitantly, an increase in hexose concentrations was observed. Thus, in these experiments, the delivery of hexoses by acid invertase activity did not limit kernel development. Differences in grain yield at maturity between salt and drought stress were most likely caused by salt‐specific effects (Na⁺ toxicity), Fabregas being more affected than Pioneer 3906.     

青土湖水面形成区土壤颗粒组成与化学特性变化

青土湖输水作为石羊河流域治理的一项关键措施,对保护湖区水资源和生态环境具有重要意义。在距青土湖水面边缘东南方向0-450 m的10个样点中分3层取0-60 cm土样,测定土壤粒径的质量百分比与全氮、全磷、全钾和电导率,分析青土湖水面形成后土壤颗粒组成与化学特性变化。结果表明,随着离水面边缘距离的增加,土壤颗粒与化学特性呈有规律的增减变化,土壤粘粉粒组成与其全磷、全钾之间存在正线性相关。青土湖水面形成加剧了距水面边缘0-150 m处的土壤理化性质变化;土壤细粒及养分出现富集,分别在距水面边缘100-150 m和300 m处达到最大值。因此,土壤养分与土壤细物质的良好相关性表明,土壤粘粉粒变化可作为反映该区域土壤性状变化和评价衡量水面形成后土壤恢复程度的定量指标之一。     

Establishment of macro-aggregates and organic matter turnover by microbial communities in long-term incubated artificial soils

The study of interactions between minerals, organic matter (OM) and microorganisms is essential for the understanding of soil functions such as OM turnover. Here, we present an interdisciplinary approach using artificial soils to study the establishment of the microbial community and the formation of macro-aggregates as a function of the mineral composition by using artificial soils. The defined composition of a model system enables to directly relate the development of microbial communities and soil structure to the presence of specific constituents. Five different artificial soil compositions were produced with two types of clay minerals (illite, montmorillonite), metal oxides (ferrihydrite, boehmite) and charcoal incubated with sterile manure and a microbial community derived from a natural soil. We used the artificial soils to analyse the response of these model soil systems to additional sterile manure supply (after 562 days). The artificial soils were subjected to a prolonged incubation period of more than two years (842 days) in order to take temporally dynamic processes into account. In our model systems with varying mineralogy, we expected a changing microbial community composition and an effect on macro-aggregation after OM addition, as the input of fresh substrate will re-activate the artificial soils. The abundance and structure of 16S rRNA gene and internal transcribed spacer (ITS) fragments amplified from total community DNA were studied by quantitative real-time PCR (qPCR) and denaturing gradient gel electrophoresis (DGGE), respectively. The formation of macro-aggregates (>2 mm), the total organic carbon (OC) and nitrogen (N) contents, the OC and N contents in particle size fractions and the CO₂ respiration were determined. The second manure input resulted in higher CO₂ respiration rates, 16S rRNA gene and ITS copy numbers, indicating a stronger response of the microbial community in the matured soil-like system. The type of clay minerals was identified as the most important factor determining the composition of the bacterial communities established. The additional OM and longer incubation time led to a re-formation of macro-aggregates which was significantly higher when montmorillonite was present. Thus, the type of clay mineral was decisive for both microbial community composition as well as macro-aggregation, whereas the addition of other components had a minor effect. Even though different bacterial communities were established depending on the artificial soil composition, the amount and quality of the OM did not show significant differences supporting the concept of functional redundancy.     

气候变化对秃尾河流域径流量的影响

为探讨秃尾河流域径流量对气候变化的关系,利用秃尾河流域1970～2005年36 a来的气温、降水和天然径流量数据,对该流域气温、降水和径流量年际和季节性的变化特征及趋势进行了分析,研究了气候因子与径流量的相关性.研究结果表明:秃尾河流域年平均气温呈现明显升高趋势,以冬季升温为主；年降水表现为缓慢减少趋势,降水减少主要表...