陇西黄土高原新石器文化与环境演变的可能联系

本文运用黄土－古土壤磁化率记录、＾１４Ｃ测年以及孢粉组合分析测试手段，研究了该地区全新世以来自然环境的演化（着重古气候的演化过程），揭示了全新世气候存在五个相对温暖湿润的古土壤发育阶段和五个相对干燥寒冷的粉尘堆积阶段。同时结合考古资料，探讨了环境变化与人类文化的产生、迁移、发展之间的可靠联系，指出古气候的变化是文化类型发生转变的重要原因之一。     

植物钙营养与贮存关系的研究

多年多点试验表明：钙在４种石灰性土壤以及一些植物体内的运输缓慢；在生殖生长为主期间，根外喷施０．４％ＣａＣｌ２溶液，可改变果实表皮细胞形状，有效地延长果品贮存期，ｔ检验处理均高于对照，差异均达极显著。     

高压静电果蔬保鲜机理分析

本对高压静电场果蔬保鲜机理进行了较为深入的分析,认为果蔬受高压静电场的作用,吸收了场能,改变了果蔬内部的能量分布,导致细胞膜电势发生变化;同时,高压电场电离周围空气产生Ｏ３,利用Ｏ３杀菌和分解果蔬中产生的乙烯的作用,破坏果蔬的后熟条件;另外,高压静电场的作用降低了苹果中生物酶的活性,使其呼吸代谢活动受到抑制,从而有效的保存水分达到保鲜效果。     

大孔径毛细管气相色谱法测定野生果汁中的氨基酸

建立了一种以正丁醇和七氟丁酸酐为衍生化试剂的氨基酸气相色谱分析法。优选了衍生化条件，对野生果汁中的氨基酸进行了分离及定量分析，经多种样品测定，均获得满意的分析结果。     

真空冷冻干燥工艺中沙棘果共晶点测定与分析

阐述了共晶点在真空冷冻干燥工艺中的重要意义,在冻干试验中采用电阻法测定不同成熟度沙棘果的共晶点温度.对试验数据进行曲线拟合,确定共晶区,并根据函数曲率的物理意义,得出成熟度为"果皮黄色"和"果皮红色"的沙棘果共晶点分别为-22 ℃和-23 ℃.     

Mite parasitism of moths: Examples of paleosymbiosis in Dominican amber

Summary Two adult moths (families Gracillariidae and Tineidae) in Dominican amber each contained a pair of larval parasitic mites attached to their bodies. The larval mites were identified as belonging to the family Erythraeidae and represent the first fossil evidence of moths parasitized by mites. Phylogenic and evolutionary implications of this find are discussed in light of similar extant associations.     

几种保鲜方法对柿子的影响

以柿子为材料,用不同试剂处理结合不同保鲜方式对柿子保鲜效果进行了研究,对调查数据进行回归方差分析和新复极差测验得出,柿子在存放过程中的烂果率及硬度的变化曲线为逻辑斯蒂曲线,用保鲜剂18^#和石灰水同时处理或丙二醇和丙三醇同时处理,能显著降低柿子烂果率并能较好地保持其硬度,贮藏方法以地窖贮存保鲜效果最好,缸存次之,空气中自然存放效果最差。     

The reconstruction of fossil planation surface in China

On the basis of results of relative subjects, the fossil planation surface has been discussed by the authors from the point of geomorphologic view. The discussion contents included the characteristic information, research methods, paleotopography (gradient and altitude) and other problems about fossil planation surface. The recognition and reconstruction of fossil planation surface mainly rely on the following characteristic information: ( i ) the character of erosion unconformity surface; (ii) the paleo-weathering crust and residual deposits; (iii) the paleo-karst and filled deposit in the paleo-karst under the unconformity surface,and (iv) the character and environment of sediment above the unconformity surface. According to the above-mentioned characteristic information, the authors recognized and reconstructed two stages of fossil planation surface on Paleo-land of North China and Yangtze Paleo-land. These two fossil planation surfaces formed from Middle Ordovician to Lower Carboniferous and from Lower Permian to Upper Permian respectively. The paleo-gradient of fossil planation surface changed within 0.31‰-1.32‰, mostly less than 1.0‰. According to the developing depth of paleo-karst, the authors considered that in Suqiao buried-hill region of Paleo-land of North China, the paleo-altitude is 300 m or so above paleo-sea-level. The authors hope that the research is in favor of discussion about rising scale and process of the Tibetan Plateau. Besides, the research of fossil planation surface can provide a theoretical base for relative research,such as the reconstruction of paleoenvironment, the evolution and drift of paleo-continent, the formation and distribution of weathering ore deposits, the reservior and prospection of oil and gas, etc.     

磁化水对果蝇生育力和寿命的影响

以果蝇为试验材料,探讨了磁化水对果蝇生育力和寿命的影响.结果发现在配制培养基时加入的适当浓度的磁化水,可提高果蝇后代的生育力和寿命.