H'/> Meteorological conditions during dust (PM<ce:inf loc='post'>10</ce:inf>) emission from a tilled loam soil: Identifying variables and thresholds
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Meteorological conditions during dust (PM10) emission from a tilled loam soil: Identifying variables and thresholds

机译:灰尘期间的气象条件(PM 10 )从耕种壤土土壤排放:识别变量和阈值

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Highlights ? Relationships between weather variables and FVPM10 were analyzed on a loam soil. ? Maximum wind speed and air humidity conditioned more significantly the FVPM10. ? Were estimated threshold values of weather variables for FVPM10. ? Crusting and surface aggregate size distribution influenced PM10 emission process. ? Weather and soil surface conditions interaction produces high variability of FVPM10. Abstract Soil wind erosion and consequent PM10 emission is a complex process that has been related to surface properties and meteorological conditions. Most of the studies have emphasized on the relationship between the surface conditions and the dust emission, in general on deserts and dry lakes or playas. Little is known about the influence of meteorological variables on PM10 emission from agricultural soils. The objective of this study was to identify the most important meteorological variables involved in the emission of PM10, identify their threshold values, and to analyze their interaction with the soil surface conditions. Measurements were made on a loam soil (Entic Haplustoll) in the semiarid Argentinian Pampa. Horizontal mass transport (Q) and PM10 emission were measured during two years on a bare and flat surface that was tilled periodically. The meteorological variables measured were: average and maximum wind speed, wind direction, air temperature, relative humidity and soil temperature. In 30% of the events, the PM10 concentration at 1.8m height exceeded the average values allowed by the World Health Organization (50μgm?3 for a 24h period). Maximum values exceeded 1000μgm?3. The slope of the PM10 concentration gradient changed between spring ? summer and autumn ? winter peri
机译:<![cdata [ 突出显示 天气变量与f v pm 10 在壤土土壤上分析。 最大风速和空气湿度更明显的是f v PM 10 估计F V pm 10 外壳和表面聚合大小分布影响PM 10 发射进程。 天气和土壤表面条件的交互产生高的变化:F V PM 10 抽象 土壤风蚀和随后的PM 10 发射是一项复杂的过程表面性质和气象条件。大多数研究都强调了表面条件和粉尘排放之间的关系,一般在沙漠和干湖泊或游戏中。关于气象变量对PM 10 农业土壤的发射的影响很少。本研究的目的是确定PM 10 ,识别其阈值的最重要的气象变量,并分析与土壤的相互作用表面条件。在半干旱阿根廷潘帕的壤土土壤(昆虫Haplustoll)上进行了测量。水平传输(Q)和PM 10 在两年内进行两年的裸露和平坦的表面上测量的发射,这些裸露的表面定期耕种。测量的气象变量是:平均和最大风速,风向,空气温度,相对湿度和土壤温度。在30%的事件中,PM 10 浓度为1.8 M高度超过了世界允许的平均值健康组织(50 μg m ?3 24 < CE:HSP SP =“0.25”/> H周期)。超过1000 μg m ?3 。 PM 10 浓度梯度在弹簧之间发生变化?夏天和秋天?冬季佩里

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