262 resultados para RAINWATER


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近几年随全球变暖和大气污染的加剧,有机气溶胶对气候和环境的影响引起了广泛的关注。其中低分子有机酸由于易溶于水,易挥发等特性可以改变大气颗粒物吸湿性、粒径分布以及形成云凝结核活性,进而改变全球的水循环和辐射平衡,而日益成为大气化学研究的重要内容。低分子有机酸极强的水溶性使雨水成为研究大气有机酸的理想载体。有机酸进入降水后是降雨的酸度重要贡献者,尤其是边远地区有机酸对降水酸度贡献高达65%。传统的大气降水研究主要侧重无机离子,认为硫酸和硝酸是降水酸度的主要贡献者,而忽略对降水中有机组分的研究。以贵阳和重庆等为代表的西南地区是我国酸雨污染的重灾区,该地区是典型喀斯特地形地貌区,生态环境具有极端的脆弱性和破坏后难以恢复性,在该地区研究酸雨形成和影响因素具有特殊的重要意义。本研究选取典型酸雨区(贵阳市)和人为污染较少黔东南州黎平县尚重镇为研究对象,2006-4~2007-4期间,收集大气降水样品221个,测定了大气降水中7种有机酸和主要阴、阳离子。对有机酸对酸雨的贡献及大气降水中无机离子和有机酸的浓度分布、变化规律、主要来源和沉降通量进行研究。主要得到了以下几点认识: 1、建立了离子色谱同时测定雨水中有机酸和无机酸分析条件。以戴安AS11-HC为分离柱、AG11-HC为保护柱,RFC-30淋洗液发生器在线产生KOH淋洗液,主要梯度条件为1mmol ( 0~6min) 、1mmol~30mmol (6~31min)。淋洗液流速1.5ml/min,柱温39℃。此条件下主要有机酸线性相关系数0.9992~0.9999,RSD%≤5%,精密度RSD%≤5%(丙酮酸RSD%=13.8%),样品的加标回收率在80~120%之间,满足分析测试要求。 2、 贵阳市降水样品pH值的分布范围为2.49~6.92,年均值为3.28。雨水酸化率为73.8%,其中pH值小于4.0雨水占样品总数42%。尚重镇降水样品pH值的分布范围为5.01~6.50,年均值为5.83,降水的酸雨率为18.4%。贵阳市酸雨污染仍十分严重,重酸雨尤为突出(pH<4.0),尚重镇酸雨污染较轻。 贵阳市降水样品电导率在10~1028μS/cm之间,平均值为248μS/cm,降水电导率高反映了贵阳市大气污染显著。尚重镇降水样品电导率在2.2~52.8μS/cm之间,平均值为18.1μS/cm,降水电导率低反映大气污染较轻。 3、贵阳市大气降水主要无机离子是SO42-、NO3-、H+、Ca2+、NH4+,雨量加权平均浓度分别为154.1μmol/L、33.9μmol/L、520.7μmol/L、226.4μmol/L和158.3μmol/L。采样期间,贵阳市H+年沉降通量为496.9mmol/m2/yr,夏季H+沉降占全年沉降总量的78%,贵阳市SO42-年沉降通量达到151.5mmol/m2/yr,有195.3mmol/m2/yr的Ca2+沉降。NH4+、Mg2+、Na+、K+、NO3-、Cl-的沉降通量分别为138.7mmol/m2/yr、50.9mmol/m2/yr、26.8mmol/m2/yr、11.4mmol/m2/yr、32.3mmol/m2/yr和12.6mmol/m2/yr。 尚重镇贵阳市大气降水主要无机离子是SO42-、NO3-、Ca2+、NH4+,其雨量加权平均浓度分别为43.1μmol/L、19.3μmol/L、33.0μmol/L和49.5μmol/L。采样期间,尚重镇[H+]年沉降通量为0.5mmol/m2/yr。SO42-、Ca2+和NH4+是发生沉降主要离子,分别为13.9mmol/m2/yr、10.6mmol/m2/yr和15.9mmol/m2/yr。Mg2+、Na+、K+、NO3-、Cl-的沉降通量分别为2.1mmol/m2/yr、5.9mmol/m2/yr、3.0mmol/m2/yr、6.2mmol/m2/yr和3.2mmol/m2/yr。 4、在贵阳市、尚重镇大气降水中共检测出7种低分子有机酸,分别是甲酸、乙酸、草酸、丙酮酸、丙酸、甲烷磺酸和乳酸。其中甲酸、乙酸和草酸是三种主要的有机酸。贵阳市甲酸、乙酸和草酸年平均浓度分别为14.24μmol/L、9.35μmol/L和2.79μmol/L,而在尚重镇它们浓度分别为4.95μmol/L、1.35μmol/L和2.31μmol/L。根据酸平衡常数计算法,贵阳市有机酸对自由酸贡献分别为:甲酸-7.9%,乙酸-4.7%,草酸-6.1%,三种主要有机酸贡献了18.7%的自由酸;尚重镇有机酸对自由酸贡献分别为:甲酸-25.1%,乙酸-7.5%,草酸-25.5%,有机酸对自由酸贡献率为58.1%。贵阳市有机酸占阴离子比值1.7~19.2%,平均值为6.6%。尚重镇有机酸对阴离子的贡献为0.5~92.2%,平均值为13.2%。有机酸对酸雨形成和大气降水化学起不可忽视的重要作用。 采样期间,贵阳市甲酸、乙酸和草酸的湿沉降通量分别为13.5mmol/m2/year 、8.9mmol/m2/year和2.6mmol/m2/year,甲酸和乙酸干沉降通量分别为26.7mmol/m2/year 和14.5mmol/m2/year,干沉降和湿沉降是贵阳市有机酸的主要沉降形式。尚重镇甲酸、乙酸和草酸的湿沉降通量分别为1.59mmol/m2/year 、0.43mmol/m2/year和0.04mmol/m2/year,甲酸和乙酸干沉降通量分别为0.1mmol/m2/year 和0.17mmol/m2/year,湿沉降是尚重镇有机酸的主要沉降形式。 5、尚重镇大气降水有机酸生长季节浓度高于非生长季节浓度,说明生长植物或土壤的释放可能是尚重镇大气有机酸的主要来源。贵阳市大气降水中有机酸非生长季节浓度高于生长季节浓度,主要原因是贵阳市降雨主要发生在夏季,降雨量的增加加大了对大气中微量气体的淋滤作用,降低了大气中有机酸浓度,同时夏季降雨pH值较低也不利于雨水对大气有机酸的溶解吸收。气象条件是影响有机酸浓度的重要因素。贵阳市大气有机酸主要在降雨初期进入降水并被清除的,降雨初期(1~2h)对大气有机酸清除占总清除的50~80%。随降雨的进行雨水中有机酸浓度逐渐降低,降雨后期略有升高,大降雨量对雨水中有机酸浓度起稀释的作用。尚重镇降雨量对有机酸浓度影响作用不明显,说明有机酸浓度不受雨量稀释作用控制,在降雨过程可能存在有机酸的液相来源。不同来源气团对贵阳市雨水中有机酸浓度影响不同,其中以北面方向气团降水中有机酸最高,与我国内陆大气污染较重有关。而源于海洋方向的东南气团雨水中有机酸浓度最低。 6、利用统计分析方法(相关性分析、主成分分析和聚类分析)和有机酸来源判别方法结合不同的来源释放有机酸通量得出:尚重镇大气中有机酸主要来源植物或者土壤直接或间接释放,而贵阳市有机酸来源相对复杂,其中植物的直接释放和机动车辆尾气排放不是大气有机酸的主要来源,生物质燃烧直接释放以及植物和人类活动向大气排放大量的不饱和有机物大气氧化可能是大气有机酸的重要来源。 7、从大气降水的电导率和pH值对比来看,贵阳市大气污染严重,雨水酸化率高,尚重镇大气污染较轻,雨水酸化率低。贵阳市大气降水中水溶性离子浓度是尚重镇的2~5倍左右,尚重镇地区酸沉降只有贵阳市0.1%,酸沉降对尚重镇不会造成太大影响。有机酸占贵阳市大气降水自由酸的19%,而尚重镇有超过1/2的自由酸是来源于低分子有机酸,是边远地区大气降水酸度的主要贡献者。来源分析表明尚重镇有机酸主要为生物源,贵阳市有机酸为人为源和生物源并重。 8、 传统的大气降水化学研究主要侧重于无机离子的研究,而忽略了对大气降水中有机组分的研究。本文第一次较全面、系统的研究了西南典型酸雨污染区大气降水化学组成以及降水酸度的来源,指出有机酸组分是西南地区大气降水化学的重要组成部分,对酸雨形成有不可忽视的影响。

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AUTHOR's OVERVIEW This chapter attempts a definition of London eco-gothic, beginning with an ecocritical reading of the ubiquitous London rat. Following Dracula, popular London gothic has been overrun, from the blunt horror-schlock of James Herbert’s 1970s Rats series to China Miéville’s King Rat. Maud Ellman’s elegant discussion of the modernist rat as a protean figure associated with a ‘panoply of fears and fetishes’, underlines how the rat has always featured in anti-urban discourse: as part of racist representations of immigration; as an expression of fear of disease and poverty; or through a quasi-supernatural anxiety about their indestructible and illimitable nature which makes them a staple feature of post-apocalyptic landscapes. Even so, the London rat is a rather more mundane manifestation of urban eco-gothic than the ‘city wilderness’ metaphors common to representations of New York or Los Angles as identified by eco-critic Andrew White. London’s gothic noses its way out through cracks in the pavements, grows from seeds in suburban gardens or accumulates through the steady drip of rainwater. However, I will suggest, in texts such as Maggie Gee’s The Flood and P. D. James’ Children of Men, London eco-gothic becomes less local and familiar as it responds to global environmental crisis with more dramatic tales of minatorial nature.

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Atmospheric inputs of mineral dust supply iron and other trace metals to the remote ocean and can influence the marine carbon cycle due to iron's role as a potentially limiting micronutrient. Dust generation, transport, and deposition are highly heterogeneous, and there are very few remote marine locations where dust concentrations and chemistry (e.g., iron solubility) are routinely monitored. Here we use aerosol and rainwater samples collected during 10 large-scale research cruises to estimate the atmospheric input of iron, aluminum, and manganese to four broad regions of the Atlantic Ocean over two 3 month periods for the years 2001–2005. We estimate total inputs of these metals to our study regions to be 4.2, 17, and 0.27 Gmol in April–June and 4.9, 14, and 0.19 Gmol in September–November, respectively. Inputs were highest in regions of high rainfall (the intertropical convergence zone and South Atlantic storm track), and rainfall contributed higher proportions of total input to wetter regions. By combining input estimates for total and soluble metals for these time periods, we calculated overall percentage solubilities for each metal that account for the contributions from both wet and dry depositions and the relative contributions from different aerosol types. Calculated solubilities were in the range 2.4%–9.1% for iron, 6.1%–15% for aluminum, and 54%–73% for manganese. We discuss sources of uncertainty in our estimates and compare our results to some recent estimates of atmospheric iron input to the Atlantic.

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This project involves the construction of a dwelling in the outskirts of Dublin City. Situated in a disused quarry, the house act as an inhabited bridge, spanning between natural and man made outcrops, service structures and a shared entrance staircase. The houses language derives from the structure necessary to achieve these spans.
The section internally is modeled to present a variety of scales of spaces. More intimate living spaces and bedrooms occur in a lower, north-facing wing. Taller living spaces address the south.

Incorporating rainwater harvesting, wood-gasifying boilers, on site wind powered electrical generation, solar thermal panels and very high levels of insulation the houses are close to energy neutral. The fact that the house is constructed in massive timber construction means that 250 tonnes of carbon are sequestered in its construction. The design includes a 25yar replanting strategy to replace the existing coniferous-forested surrounds with native species in a coppiced planting strategy to allow ongoing fuel for the house, and cash crops to be sold on.

Located in an area of outstanding natural beauty the planning and design of the house involved research into patterns of rural development, the relationship between man made interventions and the natural landscape and the technology of the vernacular. This latter research forms part of the themes being explored under the Kevin Kieran Arts Council / OPW Bursary

Aims / Objectives Questions

1 To design and construct a low energy place to dwell.
2 To investigate the relationship between man-made interventions and new construction in an area of outstanding natural beauty.
3 To derive a language of construction that is contemporary in nature but refers to precedents embedded in the vernacular.
4 To develop a low-carbon form of construction that allows the construction of the house to act to sequester carbon
5 To make a contemporary addition in sympathy with the qualities of the existing site

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Arsenic (As) contamination of communal tubewells in Prey Vêng, Cambodia, has been observed since 2000. Many of these wells exceed the WHO As in drinking water standard of 10 µg/L by a factor of 100. The aim of this study was to assess how cooking water source impacts dietary As intake in a rural community in Prey Vêng. This aim was fulfilled by (1) using geostatistical analysis techniques to examine the extent of As contaminated groundwater in Prey Vêng and identify a suitable study site, (2) conducting an on-site study in two villages to measure As content in cooked rice prepared with water collected from tubewells and locally harvested rainwater, and (3) determining the dietary intake of As from consuming this rice. Geostatistical analysis indicated that high risk tubewells (>50 µg As/L) are concentrated along the Mekong River's east bank. Participants using high risk tubewells are consuming up to 24 times more inorganic As daily than recommended by the previous FAO/WHO provisional tolerable daily intake value (2.1 µg/kgBW/day). However, As content in rice cooked in rainwater was significantly reduced, therefore, it is considered to be a safer and more sustainable option for this region.

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The 2010 Eyjafjallajökull lasted 39 days and had 4 different phases, of which the first and third (14–18 April and 5–6 May) were most intense. Most of this period was dominated by winds with a northerly component that carried tephra toward Europe, where it was deposited in a number of locations and was sampled by rain gauges or buckets, surface swabs, sticky-tape samples and air filtering. In the UK, tephra was collected from each of the Phases 1–3 with a combined range of latitudes spanning the length of the country. The modal grain size of tephra in the rain gauge samples was 25 um, but the largest grains were 100 um in diameter and highly vesicular. The mass loading was equivalent to 8–218 shards cm2, which is comparable to tephra layers from much larger past eruptions. Falling tephra was collected on sticky tape in the English Midlands on 19, 20 and 21st April (Phase 2), and was dominated by aggregate clasts (mean diameter 85 um, component grains <10 um). SEM-EDS spectra for aggregate grains contained an extra peak for sulphur, when compared to control samples from the volcano, indicating that they were cemented by sulphur-rich minerals e.g. gypsum (CaSO4⋅H2O). Air quality monitoring stations did not record fluctuations in hourly PM10 concentrations outside the normal range of variability during the eruption, but there was a small increase in 24-hour running mean concentration from 21–24 April (Phase 2). Deposition of tephra from Phase 2 in the UK indicates that transport of tephra from Iceland is possible even for small eruption plumes given suitable wind conditions. The presence of relatively coarse grains adds uncertainty to concentration estimates from air quality sensors, which are most sensitive to grain sizes <10 um. Elsewhere, tephra was collected from roofs and vehicles in the Faroe Islands (mean grain size 40 um, but 100 um common), from rainwater in Bergen in Norway (23–91 um) and in air filters in Budapest, Hungary (2–6 um). A map is presented summarizing these and other recently published examples of distal tephra deposition from the Eyjafjallajökull eruption. It demonstrates that most tephra deposited on mainland Europe was produced in the highly explosive Phase 1 and was carried there in 2–3 days.

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Trabalho de Dissertação de natureza científica para obtenção do grau de Mestre em Engenharia Civil do Ramo Hidráulica

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Dissertação de Mestrado, Engenharia e Gestão de Sistemas de Água, 4 de Março de 2016, Universidade dos Açores.

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Trabalho de Projecto de Natureza Científica para obtenção do grau de Mestre em Engenharia Civil

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Trabalho Final de Mestrado para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização de Hidráulica

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Trabalho Final de Mestrado para obtenção do grau de Mestre em Engenharia Civil

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Relatório de Estágio para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização de Edificações

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Trabalho Final de Mestrado para obtenção do grau de Mestre em Engenharia Civil