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101.
为了研究巷道风流参数的影响因素、预测风流温湿度的变化规律,结合热湿交换理论,建立了风流与围岩壁面之间热湿交换的数学模型,以及贴体坐标系下围岩内部温度场的导热微分方程;利用数值方法,将围岩内部的导热问题与影响风流参数变化的热湿交换问题耦合起来,并以大柳塔煤矿52505综采工作面为例进行计算,得到了与实测参数较为一致的模拟结果,验证了该数值方法的有效性。研究结果表明:风流温度受原始岩温、入风流温度、局部热源强度等因素的影响,风流相对湿度与入风流温、湿度以及井下湿源的数量和强度有关;巷道壁温作为将围岩温度场与风流参数之间关联起来的主要因素,对模拟结果影响较大,其数值取决于壁面与风流之间热湿交换以及围岩原始岩温。 相似文献
102.
宁南黄土高原不同土地利用模式对土壤的影响研究 总被引:5,自引:3,他引:5
宁南黄土高原采取退耕、还林、还草措施5年后,区域局部生态环境发生了较大变化。文章针对退耕后的典型土地利用方式,阐述了自然撂荒坡地、柠条(CaraganakorshinskiiKom.)灌木林地、坡耕地产生的土壤水热、养分效应,其结果对减少宁南黄土高原土壤养分流失、提高土地生产力和合理农业布局具有重要的意义。利用径流小区试验方法,研究结果表明:不同土地利用方式下土壤储水量的变化为单峰型,与雨量峰值相比,对应储水量略有滞后现象。土壤储水量整体表现为农耕地>自然荒坡>柠条林地。受植被类型影响,坡面土层温度为荒坡草地>柠条林地>农地。随坡度增加,自然荒坡土壤有机质有降低的趋势,相同坡度下(25°)自然荒坡土壤有机质平均为12.76g/kg,是农耕地、柠条林地的1.2倍和1.94倍。在3种土地利用方式下,全磷含量没有明显差异,坡耕地土壤速效磷、速效钾含量较高,柠条林地和自然荒坡速效磷、速效钾含量没有明显差异。不同土地利用方式下,Ca-P(钙结合态的磷酸盐)占无机磷总量的比例,达29.6%~59.07%,O-P(闭蓄态磷酸盐)最少,仅占4.73%~22.45%。土壤过氧化氢酶、与土壤全氮、有机质、碱解氮呈显著正相关。 相似文献
103.
利用微分扫描量热仪(DSC)准确地测定了城市生活垃圾的含水率;热重分析仪(TGA)测定了垃圾的水和低温下有机物总含量、难挥发性有机物和灼烧残渣的含量。根据量热和热量分析结果,可方便地计算垃圾的水和低温条件下易挥发性有机物含量,结合609种有机物的燃烧热,估算了垃圾的热值。 相似文献
104.
几种裸子植物胚乳愈伤组织的诱导 总被引:4,自引:0,他引:4
取裸子植物未成熟胚乳作为外植体,在改良MS、添加不同种类激素和不同浓度配比的培养基上.分别予以热激、光培养、暗培养和刻伤胚乳等多种处理进行培养.结果表明:刻伤胚乳和适时暗培养有利于愈伤组织发生;经过25~30d的培养,在ρ(NAA)=0.5~0.75mg/L、ρ(2,4-D)=0.2~0.5mg/L、蔗糖浓度5%的培养基上,油松、白皮松、青、华北落叶松以附加ρ(KT)1.0~2.0mg/L以及白、侧柏在BA与KT配合使用的培养基上,热激后暗培养,愈伤组织诱导频率可达86.4%. 相似文献
105.
调查发现广州市屋顶自然生长的维管植物有49科109属128种,植物种类较多的科为菊科、禾本科、桑科、景天科、茜草科和鸭跖草科;屋顶自然生长的植物种类数量与环境受污染程度成反比,而与周围植物的多少成正比;屋顶自然生长的植物由于长期适应屋顶的极端环境,形成了的一些独特的生态生物学特征。基于上述结果配置相应的植物组合,设计适于屋顶绿化的生态系统箱、配制相应土壤并进行技术集成,观测其生长和隔热效应。同时进行空白对照、黑网荫蓬对照、生态隔热层对照、普通土壤种植区对比试验,发现生态隔热层和生态系统箱具有成本低、易维持、隔热好、景观美的效果。 相似文献
106.
A Numerical and Field Investigation of Surface Heat Fluxes from Small Wind-Sheltered Waterbodies in Semi-Arid Western Australia 总被引:1,自引:0,他引:1
Shelterbelts are used for a variety of purposes in agricultural environments, primarily because of their ability to improve the downwind microclimate. Excessive evaporative losses from small, agricultural water supply reservoirs in semi-arid Western Australia motivated a combined numerical modelling and field investigation into the potential for using shelterbelts to reduce evaporation from these open waterbodies. A numerical model of the disturbed momentum and turbulence fields in the region modified by the wind-shelter was employed and accounted for the presence of a waterbody downwind. The model was coupled with conservation equations for heat and moisture and sensible and latent heat fluxes were estimated from the simulated momentum, temperature and humidity fields. The numerical simulations were tested against four days of field data from two experiments conducted in the agricultural districts of southwest Western Australia that measured boundary-layer evolution over a variety of small waterbodies protected by artifical and natural wind-shelters. The model provided good predictions of windspeed during neutral conditions, but inadequate specification of the upwind boundary during non-neutral stabilities resulted in the model failing to capture any sensitivity to atmospheric stability as seen in the field data. Despite this limitation, the temperature and humidity fields were adequately captured by the model, and evaporative mass flux predictions also agreed well with estimates taken from water-balance measurements. It is concluded that well-designed wind-shelters can reduce evaporation from open waterbodies by 20–30% as a result of reductions in the velocity scales responsible for removing moisture from the water surface. The model can be used to estimate the values of various shelterbelt design parameters (e.g., porosity, height) that could be applied in the field to provide optimum evaporation reductions. 相似文献
107.
108.
109.
Remote sensing of the urban heat island and its changes in Xiamen City of SE China 总被引:12,自引:0,他引:12
World-wide urbanization has significantly modified the landscape, which has important climatic implications across all scales due to the simultaneous removal of natural land cover and introduction of urban materials. This resulted in a phenomenon known as an urban heat island(UHI). A study on the UHI in Xiamen of China was carried out using remote sensing technology. Satellite thermal infrared images were used to determine surface radiant temperatures. Thermal remote sensing data were obtained from band 6 of two Landsat TM/ETM^ images of 1989 and 2000 to observe the UHI changes over l l-year period. The thermal infrared bands were processed through several image enhancement technologies. This generated two 3-dimension-perspective images of Xiamen‘s urban heat island in 1989 and 2000, respectively, and revealed heat characteristics and spatial distribution features of the UHI. To find out the change of the UHI between 1989 and 2000, the two thermal images were first normalized and scaled to seven grades to reduce seasonal difference and then overlaid to produce a difference image by subtracting corresponding pixels. The difference image showed an evident development of the urban heat island in the 11 years. This change was due largely to the urban expansion with a consequent alteration in the ratio of sensible heat flux to latent heat flux. To quantitatively compare UHI, an index called Urban-Heat-Island Ratio Index(URI) was created. It can reveal the intensity of the UHI within the urban area. The calculation of the index was based on the ratio of UHI area to urban area. The greater the index, the more intense the UHI was. The calculation of the index for the Xiamen City indicated that the ratio of UHI area to urban area in 2000 was less than that in 1989. High temperatures in several areas in 1989 were reduced or just disappeared, such as those in old downtown area and Gulangyu lsland. For the potential mitigation of the UHI in Xiamen, a long-term heat island reduction strategy of planting shade trees and using light-colored, highly reflective roof and paving materials should be included in the plans of the city planers, environmental managers and other decision-makers to improve the overall urban environment in the future. 相似文献
110.