油菜脱出物在气流中的运动分析

测定了油菜脱出物的空气动力特性，基于ADAMS研究了气流参数的变化对脱出物运动状态的影响，并对油菜脱出物在流场中的运动进行了仿真分析，选择了适合于油菜脱出物分离的气流参数，同时指出了气流清选油菜脱出物时存在的局限性。     

不同颜色粘虫板对葡萄园昆虫的诱集效应

为筛选出对葡萄害虫诱集效果好的粘虫板,选用黄色、蓝色、白色、紫色、绿色、红色、黑色和荧光色8种颜色的粘虫板对葡萄园内昆虫进行诱集试验。结果表明,共诱到昆虫7目18科22种,主要害虫有蓟马、蚜虫和叶蝉,其中蓟马数量占到昆虫总量的88.96%,天敌昆虫主要有寄生蜂、捕食性瓢虫、食蚜蝇和东亚小花蝽。紫板、蓝板和白板对蓟马的诱集效果强,黄板、荧光板和绿板次之,红板和黑板效果差;黄板对蚜虫诱集效果强,绿板和荧光板次之,黄板与其他色板之间差异显著;黄板、荧光板和绿板对叶蝉的诱集效果好,3种色板与蓝板之间差异不显著、与其他色板差异显著。白板、蓝板和黄板诱集到的天敌数量最多,占所有颜色粘虫板诱集天敌总量的69%左右。试验期间诱集到的昆虫益害比为0.036,各色板的益害比依次为黑色>荧光色>绿色>红色>黄色>白色>蓝色>紫色,其中紫板的益害比最低,仅为0.011。结合各色板的诱虫效果和益害比进行综合分析,建议选用紫板对蓟马进行诱杀,适时适量选择性使用黄板对蚜虫、叶蝉等进行诱杀。     

提高烟叶含钾量调控措施的研究初报：Ⅰ.物理调控对提高 …

在大田生产条件下,采用单株挂牌设置处理的研究方法,研究了覆膜、断根等物理调控措施对烤烟钾吸收及其在库和源中的再分配。结果指出,地膜覆盖有利于前期叶片中含钾量的积累,而打顶后揭膜对后期叶片的含钾量的提高也有一定效果;烟株顶部遮雨对含钾量影响不明显。打项时在距茎２０ｃｍ处一面断根有利于提高烟叶含钾量,但断根太多使烟株含钾量下降。     

宁都县林权抵押贷款现状、问题及对策

宁都县林权抵押贷款,是金融企业的一项新业务,对宁都县林业的发展有着极大促进作用,但存在着贷款额度小、贷款周期短、林权评估不太规范等问题.在县林权抵押贷款实践基础上,提出问题和对策建议.     

镉胁迫对尾巨桉幼苗生长和生理特性的影响

以尾巨桉(DH_32-29)幼苗为试验材料，以植株的生长指标(苗高、地径、叶面积)、生物量、根冠比、氮平衡指数(NBI)、叶绿素相对含量(SPAD 值)、丙二醛(MDA)含量和叶绿素荧光参数为指标，通过盆栽试验设置8个10~140 mg·kg^-1浓度镉(Cd)盐溶液处理，研究了不同浓度 Cd 胁迫处理下尾巨桉幼苗的形态和生理特性变化规律。结果显示：低浓度(10 mg·kg^-1)Cd 处理对尾巨桉幼苗的形态和生理特性无明显影响。当 Cd 浓度大于20 mg·kg^-1，随着 Cd浓度的逐渐增大，其对尾巨桉幼苗的伤害程度也逐渐增加，主要表现为：植株生长缓慢、生物量减小、叶绿素相对含量和叶绿素荧光参数(Fv/Fm、φPSⅡ、NP、NBI)均下降，qP 无明显变化， MDA 含量升高。Cd 浓度大于60 mg·kg^-1以上时，尾巨桉幼苗生长出现一定程度上的损伤症状和生长停滞现象。结果表明低浓度(≤20 mg·kg^-1)Cd处理下尾巨桉幼苗能正常生长，随着浓度的增大，Cd 处理对尾巨桉的形态和生理特性造成显著影响。同时结合部分桉树适生区土壤 Cd 含量调查及相关研究结果认为，尾巨桉具有一定修复 Cd 污染区土壤的潜力。     

不同氮肥用量对水稻黄华占产量及主要经济性状的影响

为充分发挥水稻黄华占高产高效潜力,本试验研究了不同氮肥用量对黄华占产量及产量构成因素的影响,结果表明:黄华占纯氮用量以180kg/hm2为宜,在土壤肥力水平较高地区种植,纯氮用量应酌减,但一般不宜低于150kg/hm2,且经济效益较高。     

凤冈县三资转换的成效与困境及对策

由资源转换成资产再转换为资本的做法简称三资转换。贵州省凤冈县充分利用农村产权制度改革试点机会,积极探索三资转换工作,在激发农村发展活力、有效解决三农问题方面产生了积极的影响。为进一步推动凤冈县的三资转换工作提供参考,在凤冈县实地调查的基础上,对三资转换的路径和成效进行了归纳总结,对三资转换工作面临的困境进行了探讨,同时提出了三资转换的对策。     

Soil organic matter fractionation as a tool for predicting nitrogen mineralization in silty arable soils

After decades of searching for a practical method to estimate the N mineralization capacity of soil, there is still no consistent methodology. Indeed it is important to have practical methods to estimate soil nitrogen release for plant uptake and that should be appropriate, less time consuming, and cost effective for farmers. We fractionated soil organic matter (SOM) to assess different fractions of SOM as predictors for net N mineralization measured from repacked (disturbed) and intact (undisturbed) soil cores in 14 weeks of laboratory incubations. A soil set consisting of surface soil from 18 cereal and root‐cropped arable fields was physically fractionated into coarse and fine free particulate OM (coarse fPOM and fine fPOM), intra‐microaggregate particulate OM (iPOM) and silt and clay sized OM. The silt and clay sized OM was further chemically fractionated by oxidation with 6% NaOCl to isolate an oxidation‐resistant OM fraction, followed by extraction of mineral bound OM with 10% HF (HF‐res OM). Stepwise multiple linear regression yielded a significant relationship between the annual N mineralization (kg N/ha) from undisturbed soil and coarse fPOM N (kg N/ha), silt and clay N (kg N/ha) and its C:N ratio (R² = 0.80; P < 0.01). The relative annual N mineralization (% of soil N) from disturbed soils was related to coarse fPOM N, HF‐res OC (% of soil organic carbon) and its C:N ratio (R² = 0.83; P < 0.01). Physical fractions of SOM were thus found to be the most useful predictors for estimating the annual N mineralization rate of undisturbed soils. However, the bioavailability of physical fractions was changed due to the disturbance of soil. For disturbed soils, a presumed stable chemical SOM fraction was found to be a relevant predictor indicating that this fraction still contains bio‐available N. The latter prompted a revision in our reasoning behind selective oxidation and extraction as tools for characterizing soil organic N quality with respect to N availability. Nonetheless, the present study also underscores the potential of a combined physical and chemical fractionation procedure for isolating and quantifying N fractions which preferentially contribute to bulk soil N mineralization. The N content or C:N ratio of such fractions may be used to predict N mineralization in arable soils.