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The result shows, grass of Sikkim small hole is temporary decline Yan period with permanent decline water content of Yan period soil is respectively 7.06% be in temporary decline with 6.20%; the Sikkim of Yan period is small after water of Kong Cao answer bibulous and rapid, decline Yan condition is eliminated gradually, appearance of aftertreatment group of answer water 6 H and contrast active of basic consistent;SOD is during threatening processing with markedder than notting have to taking a picture change, the ascendant;CAT that there is certain range after answer water and POD active are in threatening during after rising first, drop, all remarkable prep above contrasts level, and the active;MDA content that still keeps taller after answer water as the extension of time of arid and threatening processing mushroom, to threatening the 8th climate reachs maximum, content of the MDA in the lamina after answer water drops quickly, arrive the 5th day after answer water, content of the MDA in threatening group lamina is adjacent already contrast level.

结果显示,锡金微孔草暂时萎焉期和永久萎焉期土壤含水量分别为7.06%和6.20%;处于暂时萎焉期的锡金微孔草复水后吸水迅速,萎焉状态逐渐消除,复水6 h后处理组外貌和对照基本一致;SOD活性在胁迫处理期间和对照相比无显著变化,复水后有一定幅度的上升;CAT和POD活性在胁迫期间先上升后下降,均显著高于对照水平,且复水后仍然保持较高的活性;MDA含量随着干旱胁迫处理时间的延长而迅速增加,到胁迫第8天时达到最大值,复水后叶片中MDA含量迅速下降,到复水后第5天,胁迫组叶片中MDA含量已接近对照水平。

The project team has taken loess, lacustrine and peat sediments and tree ring as the research carrier, a systematic study has been carried on the warm phases of the different period (60-25 ka, last deglaciation, Holocene, the recent e few hundred years) and the last interglaciation on the basis of the extensive field investigation and laboratory analysis.

项目组以黄土、湖沼和树轮等沉积物为研究载体,经过大量的野外考察和实验室分析测试,对我国半干旱带末次间冰期和距今六万年以来不同时间段的温暖期(6万年到2.5万年、末次冰消期、全新世、最近几百年)进行了系统的研究,取得了一批重要的阶段性成果,确认了东亚季风气候和温暖期的不稳定性特征。

Under the invariable air temperature and sunlight, the relatively high precipitation influences on vegetation mainly distribute in semi-arid and arid regions. The analysis on lag correlation coefficient indicates: vegetation activities are mostly influenced by precipitation and the influence has a delay of 20 days.

从华南经华东到华中地区,随着年积温的降低,绿度始期变化不大,绿度末期提前趋势明显,绿度期逐渐缩短;由华北、陕晋经内蒙至西北地区,因水分条件的变化,干旱指数逐渐增大,绿度始期逐渐推迟,绿度末期大致提前,植被绿度期逐渐缩短。

The results suggested that properly increasing fertilizer amount is conducive to photosynthetic system recovery and water use efficiency increasing of winter wheat which are rewaterd after moderate drought stress at regreen stage.

结果提示了,冬小麦返青期中度干旱胁迫条件下,适量增施底肥有利于复水后光合系统的恢复和单叶WUE的提高,而在重度干旱胁迫条件下应适当减少基肥的施入量。

The phenophase, growth speed, structure of tussock, bloom habits, yield of new russian wildrye strain were studied, The results showed that the new strain has good traits of strong cold and drought-resistance, turning-green early, fast development and long vegetative growing period, more tillers, developed rootsystem, high yield and bloom trimly. It is suitable to being planted in arid and semi-arid region.

对新麦草新品系及对照山丹新麦草的物候期、生长速度、草层结构、开花习性、产量性状等生物学特性和生产性能的研究结果表明,该品系具有抗寒、耐旱性强、返青早、生长发育快、青绿持续期长、分蘖多、须根系发达、开花整齐和产量高等优良特点,适宜于干旱半干旱地区栽培,具有很好的推广种植前景。

The basin is one of the Cenozoic rift basins, which has experienced a series of paleo-climate change since Early Pleistocene, including wet cold, wet-warm, and arid. A former lake was believed to develop at the early stage of late Pleistocene (around 120 ka BP), and vanish during the Holocene. With the vanishment of the lake, the early Yellow River occurred. It results in a complex sedimentary environment with fluvial and lacustrine sediments interlacing each other.

河套盆地是一个新生代断陷盆地,自更新世早期以来经历了由湿冷-湿冷/暖-全新世干旱的古气候变化,盆地的发展经历了湖泊全盛期-收缩期-消亡期-河流发育期,沉积环境演化为湖积/河积交错沉积。

A pot experiment was conducted to investigate the effect of soil water on protective enzymes of superoxide dismutase, catalase and peroxidase, and also on membrane lipid peroxidation including malonaldehyde and plasma membrane permeability in pea (Pisum sativum Linn.) leaf during flowering and pod-bearing stages under drought stress and water recovery conditions. Antioxidant ability of pea during flowering and pod-bearing stages was also analyzed.

为探讨不同水分条件对豌豆保护酶系统和膜脂过氧化的影响,采用盆栽人工控水试验方法,模拟干旱胁迫及复水条件,研究了不同水分处理对花荚期豌豆叶片超氧化物歧化酶、过氧化氢酶、过氧化物酶活性以及过氧化产物丙二醛含量和脂膜相对透性的影响,并对花荚期豌豆抗氧化能力进行了综合评价。

According to the principles of synthesis, dominance, regionality and relative consistency, the environment degradation evaluation system is divided into three classes: vulnerable region, vulnerable type and vulnerable cell. The research area belongs to the erosion degraded Southern Red Hilly Area region. Based on the conceptions and grading, the dissertation probes into the methodology of evaluation and case study, and establishes a potential degradation evaluation system which comprises altitude, gradient, soil erosion index K, annual rainfall, the proportion of rainfall in raining period, and the drought index of rainless period.

在脆弱性概念及其分类的基础上,本文进行了脆弱性评估的方法探讨和实证研究,在脆弱性分析的基础上,选择高度、坡度、土壤可蚀性K值、降雨量、暴雨量、多雨期降雨比重和少雨期干旱指数为潜在脆弱度指标;选取作为区域人地关系、社会经济发展与管理水平综合影响结果的人类活动指标森林覆盖率和坡耕地指数作为现实脆弱度评估的人为加速侵蚀的修正指标,计算生态环境的现实脆弱度,并将其指标体系与方法用于衡阳盆地生态环境脆弱度评估的实证研究。

Drought stress weakened the rhizosphere effect of ammonifying bacteria.Under drought stress,rhizospheric ammonifying bacterium amount of Baidan31 was very significantly different at seedling and jointing,and significantly different at tasseling-anthesis from that of control.Rhizospheric nitrifying bacteria tended to increase under drought stress.

干旱胁迫减弱了玉米氨化细菌的根际效应,与对照根际氨化细菌数量相比,白单31在苗期和拔节期根际氨化细菌数量受干旱胁迫的影响达极显著水平,在抽雄~开花期达显著水平;根际硝化细菌数量在干旱胁迫下有所增加。

Maize plants were treated by the low temperature under different water conditions during seedling and tasseling periods in the artificial climate chamber to determine the impacts of low temperature, drought and their combination on maize yield in the Northeast China. Based on the results of the controlled experiment, the WOFOST model was applied to simulate the integrated impacts of low temperature and drought on maize yield.

在玉米苗期和抽雄期利用人工气候箱对不同水分条件下的玉米植株分别进行低温处理,通过控制试验分析了低温、干旱以及二者合并对玉米生产的影响,在此基础上应用WOFOST作物模型模拟分析了低温、干旱以及二者合并对东北地区玉米产量的影响。

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