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本文以某市配电系统为主要研究对象，通过与国内外配电系统可靠性数据的对比，找出该配电系统在网络结构，设备可靠性及运行管理方面的不足，提出提高其可靠性的技术与管理措施。 相似文献
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Timing, duration, and transitions of the last interglacial Asian monsoon 总被引：16，自引：0，他引：16
Yuan D Cheng H Edwards RL Dykoski CA Kelly MJ Zhang M Qing J Lin Y Wang Y Wu J Dorale JA An Z Cai Y 《Science (New York, N.Y.)》2004,304(5670):575-578
Thorium-230 ages and oxygen isotope ratios of stalagmites from Dongge Cave, China, characterize the Asian Monsoon and low-latitude precipitation over the past 160,000 years. Numerous abrupt changes in 18O/16O values result from changes in tropical and subtropical precipitation driven by insolation and millennial-scale circulation shifts. The Last Interglacial Monsoon lasted 9.7 +/- 1.1 thousand years, beginning with an abrupt (less than 200 years) drop in 18O/16O values 129.3 +/- 0.9 thousand years ago and ending with an abrupt (less than 300 years) rise in 18O/16O values 119.6 +/- 0.6 thousand years ago. The start coincides with insolation rise and measures of full interglacial conditions, indicating that insolation triggered the final rise to full interglacial conditions. 相似文献
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- 1. Current monitoring strategies of governmental organizations tend to be focused on relatively large flowing and standing waters, and until recently those polluted by point sources. Consequently areas of high conservation interest tend to be understudied, and defining reference conditions, as required by current legislation, is difficult to achieve.
- 2. In order to address this imbalance, water samples have been collected and analysed once in each of four seasons during 2003 from 72 locations within a 100 km2 area of the oligotrophic River Spey catchment in NE Scotland. The sampling design included examples of running water (headwater streams and the main rivers) and standing water (lochs, lochans, pools, ditches, backwaters, bogs). Altitude ranged from 220 to 980 m and incorporated a climatic regime from cool temperate to sub‐alpine. Each sampling campaign targeted low‐flow conditions to evaluate steady‐state nutrient concentrations.
- 3. Concentrations of the major soluble nutrients nitrogen and phosphorus demonstrated high spatial and temporal variability, with soluble organic and molybdate unreactive forms generally being dominant. Concentrations of ammonium‐N, nitrate‐N and soluble reactive phosphorus were extremely small, with 50% of samples falling below 8, 5 and 1 µg L?1, respectively, during spring and summer.
- 4. Sampling sites were grouped either by water‐body type or by the properties of their immediate biophysical zone. Together these two groupings explained 33–38% of the variance in water chemistry. Certain changes were detectable across most habitats and biophysical zones.
- 5. A decline in the concentration of nitrate that occurred in reaches downstream from certain headwater streams draining the mountain areas indicated the potential for its within‐stream utilization. Inorganic N dynamics differed between small streams and large rivers.
- 6. Landscape‐scale patterns were recorded in spring and summer nutrient availability with inorganic N and P thresholds (arbitrarily defined) of 10 and 1 µg L?1, respectively.
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Wheat grown in Gabalong soil was examined for the microflora of its seminal and nodal root systems of similar age. At all stages of sampling, the seminal roots were found to support a significantly-larger population of bacteria, actinomycetes and fungi in their rhizosphere than the nodal roots. The seminal roots had higher numbers of bacteria and actinomycetes in their residues, but fungal numbers were not significantly different. The “rhizosphere effects” of the two root systems, in the combined analysis, were significantly different only for fungi. An interesting trend on both root systems was that while the numbers of bacteria, actinomycetes and fungi in the rhizosphere decreased with root age, their numbers in the residue increased with age. 相似文献
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