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41.
暴雨预报的力子天气学模式和应用实例(英文) 总被引:2,自引:0,他引:2
[目的]对2010年湖南汛期13次暴雨过程进行力子天气学分析。[方法]采用力子天气学原理,通过对2010年出现在湖南的13次区域性暴雨天气过程进行合成分析。[结果]2010年湖南汛期的13次暴雨都与自组织的辐合水气流密切相关,暴雨是自组织辐合水汽流爆发后所产生的必然结果;自组织辐合水汽流的孕育区对应未来12-36小时出现暴雨的区域;自组织辐合水汽流孕育区一旦消失,则未来12-36小时不会有区域性暴雨出现;自组织辐合水汽流孕育区产生在大尺度南北力子偶的交汇域。[结论]南北力子偶是否存在可以作为汛期区域性暴雨的短期预报模式。 相似文献
42.
分析了当代名胜古迹的设计特质,在充分认识名胜古迹户外游憩空间特征的基础上,指出当前名胜古迹规划设计存在的路线设计混乱,文脉缺失,设计形式主义泛滥等问题。以崂山太清游览区的设计为例,探讨名胜古迹的营造手法。强调要尊重历史,延续文脉;适度开发,营造良好生态;合理设计路线,注重游憩者的感受;遵从美学原则,境由心生。以期使今后的名胜古迹的设计工作更具有针对性和可操作性。 相似文献
43.
44.
《Communications in Soil Science and Plant Analysis》2012,43(15-20):2249-2264
Abstract Australia's reef water quality protection plan has a key objective: “reduce the load of pollutants from diffuse sources in the water entering the Reef.” This article reports on a survey to assess the contemporary phosphorus (P) status of fertilized cropping soils across 21 catchments in coastal Queensland, Australia. The survey focused on surface soils from cane farms, vegetable and subtropical/tropical fruit tree sites. There were sampling depth effects on P levels in sugar and fruit tree sites (lower with depth). Importantly, 84% of 105 sugarcane sites were excessively fertile and only 3% rated low (P deficient). Some 75% of 16 vegetable sites and 38% of 8 fruit tree sites had excess ratings for extractable soil P fertility. Highest total P levels (0–10 cm) occurred in fruit tree sites, followed by vegetable and sugarcane soils. There are regional differences in P soil fertility, and the recycling of mill by‐products needs attention. Part 2 (Bloesch and Rayment 2006) examines the potential of these soils to release soluble P in a nutrient‐sensitive area. 相似文献
45.
张履祥农业知识传播与交流的典型耕读士人,他农业知识的来源以及自己农业知识的外传,进一步说明以他为代表的太湖地区底层士人对农业知识传播的贡献。张履祥和其生活范围内人士通过书信等方式的交流,通过这个过程把农业知识介绍给他人。这里介绍了张履祥获得农业知识的方式,包括书籍、实践、老农、家传等途径不断积累自己的农业知识。其次说明了张履祥通过血缘、地缘、结社交游、门人训导的方式将自己总结的农业知识传播出去。这个过程正是一种典型的农业知识传播方式,身为士人的张履祥是农业知识传播的纽带。 相似文献
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47.
The influence of native vegetation clearing and different further soil managements on fungal propagule population diversity
was studied in the present work. In each of the 3 years (1998, 1999, and 2000), soil samples were collected at the depth of
0–7.5 cm from sites under native vegetation (V0); naturalized prairie, cleared in 1982 (P16); conventional tillage, cleared
in 1972 (T26); and direct drilling, cleared in 1958 (D40). Fungal population size and relative abundance of fungal genera
were studied by plate counts and further identification of isolates on potato dextrose agar. The undisturbed site and the
other sites with increasing time elapsed since native vegetation clearing and different management history showed a distinctive
distribution of fungal genera. There were significant differences (p<0.05) among the sites in the abundance of fungal genera analyzed in all the 3 years. Principal component analysis based on
relative fungal genus abundance differentiated the sites with 75% variance explained by the first and second components. Diversity
and abundance of isolated fungal genera were increased as density of Penicillium spp. decreased, suggesting a competitive effect of this fungal genus. The largest diversity was found in the site under no-till
management. The different distribution and relative abundance of the fungal genera studied seemed to be influenced strongly
by the management and the presence of surface residue in the no-tilled site. 相似文献
48.
Deficiency of sulfur (S) is becoming widespread in the rainfed systems of India, and there is increasing need for diagnosing the deficiency. Calcium chloride and Ca phosphate are commonly used for extracting available S in soils. Because of cost and the ease of availability locally, we prefer using Ca chloride as an extractant over Ca phosphate, for extracting available S. However, there is paucity of data on the comparative evaluation of the two extractants to extract available S, especially in soils having a wide range in natural pH (from acidic to alkaline range). It is recognized that soil pH plays a dominant role in the adsorption–desorption and extractability of sulfate‐S in soils. We compared the extraction of S by Ca chloride and Ca phosphate in 86 Indian soils having a wide range in pH (4.5 to 10.6). Sulfur in the extracts was determined by ICP‐AES. Considering all the 86 soil samples tested, there was an excellent agreement between the values of extractable S determined by using the two extractants (r = 0.96, p < 0.001). However, the correlation coefficient (r) between the values of extractable S by the two reagents, although highly significant, varied among the groups of soil samples according to the range in soil pH. The highest correlation coefficient (r = 0.99, p < 0.0001, n = 17) was found for soils with pH in the alkaline range (8.5–10.6), and the lowest correlation coefficient (r = 0.71, p < 0.0001, n = 58) was obtained with a set of soil samples with pH in the acidic range (4.5–6.5). For soil samples having pH in the near‐neutral range (6.7–7.3), an excellent agreement was observed (r = 0.93, p < 0.0001, n =11) between the extractable‐S values obtained by the two extractants. While Ca phosphate extracted higher amount of S compared to Ca chloride in soil samples with pH in the acidic range, the two extractants were equally effective for soil samples with pH in the neutral or alkaline range. Our results suggest that for most of the soils in the semiarid tropical regions, which have pH in the neutral to alkaline range, Ca chloride can replace Ca phosphate as an extractant for removing available S in such soils. 相似文献
49.
Wim Salomons 《Journal of Soils and Sediments》2005,5(1):2-8
- Dedicated to Prof. Dr. Ulrich Förstner on his 65th birthdayBackground Sediments pose problems at their deposition sites when there is too little sediment (e.g. wetlands) or too much sediment (e.g. navigable waterways) and, additionally, when they are contaminated. These problems often have their origin upstream in the river catchment. Objective Global aspects of changes concerning sediment quantity and quality, as they affect downstream areas, are reviewed. A case study of estuarine sediments demonstrates how a holistic approach helps in understanding and predicting their present and future quality. Results and Conclusions Globally, large reservoirs intercept between 25 and 30% of the sediment and consequently supply the coast with impacts on wetlands and coastal morphology. In estuaries, the composition of sediments is determined by the mixing of marine sediments supplied from the coast and the supply by rivers. Natural tracers can be used to predict mixing ratios of marine to fluvial sediments in estuaries, and hence their contamination. Scenarios on implementation of pollution abatement, the implementation of regulations as well as climate change are needed to predict future sediment quality in downstream areas. The results show, even for a ‘green’ scenario, that sediment quality in the Rhine catchment will pose future problems due to the temporal storage of contaminants in soils and sediments.Recommendations and Outlook The current methods applied make use of existing models linking sediment transport with point and diffuse sources in the river catchments and scenarios on the development of strength of point and diffuse sources. However, more effort is needed to come to a uniform framework which includes land use changes and links with more advanced scenario methodology for long to medium-term management of sediment quality and quantity in river catchments. 相似文献
50.