Factors influencing seed reserve utilization during seedling establishment in maize inbred lines

Strong seedlings are essential for high yield. To explore the foundation of strong seedlings, we investigated various factors influencing the conversion and distribution of seed storage reserves during seedling establishment in maize inbred lines. Three maize inbred lines were used to explore the effects of seed size, seed vigor, illumination duration, temperature, water content, and salt concentration of the seedling medium on the utilization of seed storage reserves during seedling establishme...     

Soil saturation effects on forest dynamics: scaling across a southern boreal/northern hardwood landscape

Patch modeling can be used to scale-up processes to portray landscape-level dynamics. Via direct extrapolation, a heterogeneous landscape is divided into its constituent patches; dynamics are simulated on each representative patch and are weighted and aggregated to formulate the higher level response. Further extrapolation may be attained by coarsening the resolution of or lumping environmental data (e.g., climatic, edaphic, hydrologic, topographic) used to delimit a patch.Forest patterns at the southern boreal/northern hardwood transition zone are often defined by soil heterogeneity, determined primarily by the extent and duration of soil saturation. To determine how landscape-level dynamics predicted from direct extrapolation compare when coarsening soil parameters, we simulated forest dynamics for soil series representing a range of drainage classes from east- central Maine. Responses were aggregated according to the distribution of soil associations comprising a 600 ha area based on local- (1:12,000), county- (1:120,000) and state- (1:250,000) scale soil maps. At the patch level, simulated aboveground biomass accumulated more slowly in poorer draining soils. Different soil series yielded different communities comprised of species with various tolerances for soil saturation. When aggregated, removal of waterlogging caused a 20–60% increase in biomass accumulation during the first 50 years of simulation. However, this early successional increase and the maximum level of biomass accumulation over a 200 year period varied by as much as 40% depending on the geospatial data. This marked discrepancy suggests caution when extrapolating with forest patch models by coarsening parameters and demonstrates how rules used to rescale environmental data need to be evaluated for consistency.     

宁波市农业自然资源及其可持续利用

从宁波市农业自然资源形成的自然地理环境基础着手,分析了宁波市农业自然资源的基本特征,进一步论述了宁波市在开发利用农业自然资源中存在的主要问题,并针对这些问题提出了宁波市农业自然资源可持续利用的若干对策。     

海湾泥碱渣和粉煤灰作为园林种植基质的氮素生理类群及生化作用研究

海湾泥、碱渣和粉煤灰是天津滨海地区大量存在的固体废弃物,通过前期室内配比筛选、盆栽试验、田间试验表明其混合基质可以用于园林绿化,并在防护林建设中获得成功.以滨海盐土、客土绿地为对照,对通过脱盐、培肥、种植毛白杨、刺槐、洋白蜡、金银木、紫花苜蓿等园林植物后基质的氨化细菌、好气性自身固氮菌、硝化细菌、反硝化细菌、纤维素分解菌等土壤氮素生理类群的数量进行了研究,同时对呼吸作用、氨化作用强度以及二者与土壤微生物数量、理化性质进行了相关性分析.结果表明,基质的氮素生理类群数量高于或与客土绿地相当,明显高于滨海盐土.呼吸作用高于客土绿地和滨海盐土,氨化作用强度与客土绿地相当,说明混合基质的氮素转化、有机物质的矿化能力以及基质整体的代谢水平好于客土绿地.土壤呼吸作用强度与土壤盐分呈极显著负相关,与细菌数量呈显著正相关.氨化作用强度与全氮、全磷、有机质含量、细菌和真菌数量呈极显著正相关,与放线菌呈显著正相关,与速效钾、盐分呈显著负相关.     

莫比朗在柑桔和土壤中的残留动态研究

采用田间试验方法,研究了莫比朗在柑桔和土壤中的消解动态和最终残留。样品用乙腈提取,过Envi-Florial固相小柱净化,液相色谱紫外检测器检测,外标法定量。残留动态试验结果表明,施药浓度为推荐剂量的两倍时(有效成分120g·hm-2),莫比朗在柑桔中的半衰期分别为7.00～8.90d,土壤中为4.00～6.38d。在有效成分为60g·hm-2的剂量下,施药3次,施药后第21d柑桔中莫比朗残留量低于0.10mg·kg-1。     

负水头条件下的水平一维土壤吸渗特征

该文分析了不同负水头条件下土壤水分运动特征,并通过室内模拟试验研究了不同负水头条件下水平一维土壤的吸渗特征,根据Brooks-corey模型推求了描述负水头条件下土壤吸渗公式,并分析了各参量间的函数关系。分析了Philip吸渗公式在负水头条件下的适用性,并对所建立的公式进行检验。研究结果表明：上述理论关系可以很好描述负水头条件下水平一维土壤吸渗过程。     

提高中文社科纸质型期刊利用率的管理探索

文章从三个方面对如何提高中文社科纸质型(或印刷型)期刊利用率的管理进行实践探索,取得良好效果进行阐述。     

作物吸收Cd的影响因素分析及籽实Cd含量的预测

我国许多大的江河流域冲积平原土壤普遍存在重金属Cd异常,食用生长在其上的粮食是人体摄入Cd的一个主要途径。作物吸收Cd量受很多土壤因素的控制,为了确定影响作物籽实Cd含量的土壤理化指标,采用多元线性回归分析对采自江苏省南京、扬州和苏州郊区的水稻和小麦籽实及相对应的土壤样品进行了研究。结果表明,土壤总Cd含量和pH值是影响农作物籽实Cd含量的两个主要因子,虽然其他土壤理化性质指标对作物吸收Cd量也有一定的影响,但是影响程度均没有达到极显著水平,在忽略这些因子的情况下,水稻和小麦籽实的Cd含量、土壤总Cd含量和土壤pH值之间具有以下相关关系：log（水稻Cd）=-0．369—0．068pH＋0．153log（土壤Cd）;log（小麦Cd）=0．624—0．164pH＋0．421 log（土壤Cd）。这两个模型对水稻和小麦籽实Cd含量的预测能力均达到了极显著水平。     

红壤干旱过程中剖面水分特征与土层干旱指标

农田水分管理以及产量评估都需要对土壤作物受旱状况定量化和指标化。干旱强度和干旱程度结合才能完整地描述土壤作物干旱状况,土壤干旱强度I是土壤剖面失水速率的函数,干旱影响逐渐累积并增强就构成干旱程度D,据此提出了包含I和D二个指数的土层干旱指标表达模式。通过红壤小区种植玉米并在抽穗期开始设置连续干旱12～36 d等6个不同的处理,研究了红壤干旱过程中剖面水分特征和干旱指标。结果表明：供试红壤干旱过程中剖面40 cm以下含水率下降幅度很小,玉米主要利用了0～40 cm土层的水分,监测30～40 cm土层含水率的变化情况可以指示玉米受到干旱胁迫的程度。连续干旱25 d后40 cm以下土层含水率明显降低,玉米产量也显著下降,此时0～60 cm土层和30～40 cm土层的干旱程度D均为0.55,可用此指标作为灌溉的依据。     

海南不同母质橡胶人工林土壤微生物群落功能特征

本研究运用Biolog-Eco微平板培养技术对海南橡胶人工林4种母质(花岗岩、玄武岩、变质岩和浅海沉积物)发育土壤微生物群落功能特征进行研究,同时测定土壤理化特性,探究不同母质发育橡胶人工林土壤微生物群落的代谢活性和功能特征及其与土壤理化性质的相关性.结果表明:不同母质之间橡胶人工林土壤理化性质存在显著差异,总体上玄武...