毕节地区各土类水土保持树种的Fuzzy评价

根据毕节地区16个主要造林树种的生态生物学特性,结合本区气候和土壤生态条件,运用 Fuzzy 二级评价模型,对各土类水土保持树种的适宜程度进行了综合评价。     

张家界气候资源的利用与保护

为了充分开发利用和保护张家界的气候资源,我们采用长期定点和短期定位相结合的方法,观测研究了张家界的气候和森林小气候特征。研究证明,张家界具有亚热带湿润季风气候区的山地气候特征,森林小气候舒适宜人,旅游气候资源和农业气候资源丰富,应大力发展旅游业和林业;保护森林植被是保护张家界气候资源的关键。     

国外厌氧颗粒污泥培养研究简介

本文荟萃了荷兰、美国、德国、法国许多学者对厌氧颗粒污泥培养的研究，强调了颗粒化的机理仍是一个较为复杂而尚存在许多未知数的领域，并介绍了颗粒污泥的贮存。     

论我国重大危险源辨识标准

简要介绍了国外重大危险设施的辨识标准研究情况,并结合我国重大危险源普查试点工作的初步辨识标准,以及几个试点城市普查的数据分析,提出了我国重大危险源辨识最小标准的建议     

居室放射性

本文介绍了放射性的来源,讨论了室内γ射线和氡及其子体,计算了相关的年剂量当量     

广元飞播造林成效与流域生态环境效益研究

运用川北广元历年飞播成效调查以及固定标准地观测的结果,结合笔者从事飞播造林技术与管理工作的经验,得出：飞播造林是速度快、省劳力、投资少、成本低、效益高的造林方式,推广飞机播种造林是绿化川北山地,迅速治理流域生态环境和实现山区经济可持续发展的有效措施     

由震洪相关回顾性预测1870年长江特大洪水

１８７０ 年长江特大洪水是多因叠加和强化的结果, 因之要预测它也要从各方面去研究。如特大洪水前的先行降雨和洪水所反映的大气环流状况及太阳活动情况等。本文把１９３１ 年、１９５４年、１９９１ 年长江大洪水前一年内缅甸北部有７ 级以上大震及１９９８ 年长江大洪前一年内缅北有６级左右震群集中活动的相关指标移用于１８７０ 年长江特大洪水前, 发现其前一年, 即１８６９ 年缅北亦有７ 级以上大震发生。震洪相关的物理机制是与地震活动有关的地下放气使孟加拉湾向长江流域输送的水气更多,如遇北方冷气团南下则降大雨致洪。另外,１８７０ 年长江洪水之所以比１９３１ 年、１９５４ 年、１９９１ 年和１９９８ 年长江洪水还大, 我们认为１８７０ 年４ 月１１ 日在长江上游山区有７ 级以上大震发生, 且震前有大雪发生, 是叠加在前述致洪因素上的另一因素。     

通才式安全工程专业课程设置的探讨

根据安全工程专业所处的学科结构体系 ,讨论了通才式安全工程专业高等教育课程设置所考虑的因素。提出了通才式安全工程专业高等教育课程的设置思想、专业基础课和主干课的学时比以及实践与理论相结合的实习方法。     

Characteristics of bricks made from waste steel slag

The characteristics of bricks made from steel slag were investigated in this research. Slag addition was shown to reduce the required firing temperature. When the firing temperature was greater than 1050 degrees C and the slag addition less than 10%, the bricks met ROC national standard CNS 3319 third-class brick for builders. The percentage of slag increased as the quartz and kaolin decreased in the sintered samples while the magnesium aluminum silicate and calcium silicate increased. There were no new crystal phases observed in these samples.     

Interactions of chlorpyrifos with colloidal materials in aqueous systems

An understanding of sorptive processes is key to describing the fate of chlorpyrifos [O,O-diethyl-O-(3, 5, 6-trichloro-2-pyridyl) phosphorothioate] in aquatic environments. The objectives of this study were to evaluate isotherms for adsorption and desorption of chlorpyrifos on colloidal materials and to advance understanding of interaction mechanisms between chlorpyrifos and colloidal materials. Six Ca-saturated reference smectites, one Ca-saturated humic acid (Ca-humate), and one suspended sediment sample, collected from the Upper Cedar River, Iowa, were studied. A batch equilibration technique was employed to quantify adsorption and desorption isotherms for chlorpyrifos over the 0 to 100 microg L(-1) concentration range in a 0.01 M CaCl(2) background. Large differences in sorption affinity and variation in desorption hysteresis were found among the smectites. Neither chlorpyrifos adsorption nor its desorption were correlated with cation exchange capacity, surface area, or surface charge density of the smectites. The evidence suggests that physical interaction between chlorpyrifos and smectites is the dominant mechanism for adsorption of chlorpyrifos in aqueous systems. Chlorpyrifos was very strongly sorbed on Ca-humate and was not desorbed from the Ca-humate back into the aqueous solution. Chlorpyrifos was moderately sorbed on river sediment, and a large adsorption-desorption hysteresis was also found. The study implies that the nature of both organic and inorganic materials in suspended sediment can influence the adsorption-desorption behavior of chlorpyrifos in aqueous systems.