长期培肥对土壤酶活性的影响

25a的有机肥长期定位试验地中土壤养分和有关酶活性研究表明:耕种和不同的培肥方式均能提高土壤养分的含量,明显地改善土壤的生物活性,其中对土壤脲酶和磷酸酶活性影响明显,多酚氧化酶显著性则较差。对土壤酶活性进行相关分析发现,土壤脲酶和碱性磷酸酶之间呈极显著正相关,且这两种酶与有关主要土壤肥力因子均呈显著或极显著正相关关系。揭示出了土壤脲酶和碱性磷酸酶活性可以用来作为评价土壤肥力的综合指标。     

人为影响下古尔班通古特沙漠小尺度生态环境变化

随着沙漠中油气资源勘探开发、公路建设和重大工程相继实施 ,对生态环境的人为影响日益加深。本文以重大工程实验点为例 ,通过研究对比工程影响区内人工沙垄和自然沙垄的砂质新成土理化性状和植被群落特征 ,指出了沙漠生态环境在人为干扰下发生的一系列变化 ,以及受损生态环境在人们采取积极补救措施的情况下所具有的自然修复能力     

Spatio-temporal modelling of broad scale heterogeneity in soil moisture content: a basis for an ecologically meaningful classification of soil landscapes

We describe the classification of landscapes characterised bymineral soil using a model that calculates soil moisture availability on amonthly basis. Scotland is used as a case study area. The model uses potentialsoil moisture deficit, estimated using broad scale (40 × 40 km)climate patterns, in conjunction with meteorological station measurements toobtain finer scale values of climatic soil moisture deficit. Point estimates ofsoil available water are obtained for soil characteristics using appropriatepedotransfer functions, and geostatistical techniques are used to upscale theresults and interpolate to a 1-km grid. Known heterogeneityin soil physical characteristics is used to provide local corrections to thepotential soil moisture deficit, estimated using the climatic variables above.Temporal profiles of monthly water content are modelled for each1-km location and classified into six classes usingunsupervised cluster analysis. The spatial distribution of these classesreflects regional variations in the availability of moisture and energy, onwhich finer-grained topographic patterns are superimposed. In the case study,the broad scale spatial heterogeneity of heathlands and grasslands on mineralsoils in Scotland is shown to be strongly related to the soil moistureclassification. The results can be used in studies investigating the patternsofdistribution of communities at the landscape and regional scale.This revised version was published online in May 2005 with corrections to the Cover Date.     

Inconspicuous restraint of rice seedling growth by root-infecting fungi in soil of a rice paddy field

 Rice seedling growth, estimated by plant height and root development and discoloration, was better in pasteurized soil than in unpasteurized soil obtained from a flooded rice field. Rice seedlings also grew better in sterilized soil modified by adding roots harvested from the pasteurized soil than in soil modified by adding roots harvested from the unpasteurized soil. The results demonstrate that seedling growth in the rice field soil was inhibited by soil microorganisms, even though no typical symptoms such as seedling blight or damping-off appeared. Pythium aristosporum is suggested to be involved in the inhibition. Thus, it appears that inconspicuous restraint of rice seedling growth could occur in soils of rice paddy fields. Received: May 20, 2002 / Accepted: October 16, 2002 Acknowledgments The authors thank Dr. T. Ichitani, former professor at Osaka Prefectural University, for providing an isolate of Pythium aristosporum for comparison, and Mr. Mitsuaki Sato of Akita Prefectural College of Agriculture for technical assistance.     

纳米微粒材料生物学活性研究进展

综述了纳米微粒的生物学效应及其免疫调节、抗菌、抗肿瘤等多种生物学活性.     

退化草地群落演替趋向研究进展

草地群落的退化演替以植物个体、种群与群落层次上植物的动态以及土壤理化性状的改变等现象为表征。主要从植物个体形态特征、草地退化模式、草地土壤养分变化等方面对退化的响应,探讨了草地退化演替的特征和趋势,建议今后对草地的退化演替机理、放牧生态学、恢复生态学、界面生态学及草地的价值评估等方面进行更深入的研究。     

日光温室土壤盐分和养分的变化趋势

对种植 1～ 8a的日光温室土壤盐分和养分进行了调查研究 ,结果表明 ,随着日光温室种植年限的延长 ,土壤可溶性盐、电导率、养分含量呈增加趋势 ,酸碱度 (pH)呈降低趋势 ,有机质含量增幅不大 ;土壤速效养分中硝态氮含量过高 ,速效磷含量也很丰富。最后提出了温室土壤培肥和管理措施。     

不同覆土深度对鸡腿菇子实体产量的影响

本试验研究 11种覆土深度对鸡腿菇子实体产量影响。结果表明 ,不同覆土深度对子实体产量、有效子实体数和幼蕾数均存在显著的影响。覆土越厚 ,幼蕾数越少。当覆土深度在 0 5～ 3cm时 ,子实体产量和有效子实体数随着覆土层的加厚逐渐增加 ,在覆土深度为 3cm时达到最大值 ,覆土深度大于 3cm时 ,则随着覆土层的加厚而逐渐减少。从生产的角度看 ,覆土 3cm是比较适宜的覆土深度 ,此时的子实体产量最高。     

噻二唑基-3-哒嗪酮类化合物的合成及生物活性

将取代的二酰基肼环合后,得到中间体2-芳基-5-氯甲基-1,3,4-噻二唑,然后与2-叔丁基-4-氯-5-羟基-3(2H)-哒嗪酮反应,合成了8个未见文献报道的含噻二唑基哒嗪酮类化合物,其化学结构经1H NMR、高分辩质谱和元素分析确认。生物活性测试结果表明,部分化合物对粘虫P.separate W.有较好的抑制生长活性,其中化合物 3b 的EC50值为21 mg/L。     

137Cs示踪法在东北松嫩平原土壤侵蚀定量评价中的应用

根据不同退化程度草原和不同开垦年限农田土壤137Cs放射强度分析结果表明:与轻度退化草原相比,中度退化和重度退化中的137Cs放射强度分别下降了21%和52%。草原土壤开垦后,137Cs放射强度明显下降,开垦7年、15年、33年后,137Cs的放射强度分别只有轻度退化草原的37%、31%和26%。相关分析表明,伴随着土壤侵蚀的发生,土壤有机质含量、全N含量以及阳离子交换量下降。137Cs放射强度与土壤有机碳、土壤全N、交换性K和阳离子交换量呈极显著的正相关。