基于热湿交换理论的巷道风流温、湿度影响因素研究

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。     

水稻田的甲烷释放特性及其生物学机理

本文报导采用土柱法和田间原位法研究渍水稻田甲烷释放特性的结果。不同生育期的测定表明,早稻以分蘖盛期时释放量最大,以后逐渐减少,晚稻从分蘖始期起逐渐增加,至分蘖盛期、末期时达到最大,随后在孕穗期急剧减少,至生长后期又有所回升。以原位法测定表明,晚间和上午释放的甲烷量较多,中午几乎无甲烷释放,下午又有少量释放。不同施肥区稻田甲烷释放量明显不同,以施猪粪有机肥区为最高,次为施尿素无机氮区,不施肥区最低。但各施肥区水稻不同生育期的甲烷释放趋势完全一致,以分蘖期释放量最大,稻田释放的甲烷主要是稻植株释放的,可占总释放量的85％以上。行株间土壤释放的量不多。田间水释放极少,就植株而言,甲烷释放部位主要是在与土壤密切结合的未扰动的根基和根系部位,水面下茎秆白色部分和水上绿色部分几乎无释放。根系也主要是靠近根基的上半部分,根尖部位甲烷形成活性明显小得多。且研究表明,产甲烷细菌附存于根表而不进入根内组织。根际土壤中产甲烷细菌、厌氧性纤维素分解细菌和甲烷氧化细菌的数量以及总挥发有机酸含量都明显高于和行间土壤。     

杭州市城市和郊区表土磷库及环境风险评价

杭州市城市和郊区土壤磷素具有明显的积累特征并有较高的潜在释放能力。可提取态P(包括H2O-P、NaHCO3-P.NaOH-P和HCl-P)平均在80％左右，其中以HCl—P的比例最高，平均约55％。32个研究土样中，26个土样的水可溶性(H20—P)在10mg／kg以上，15个土样的NaHCO3—P在100mg/kg以上。酸性条件下P的释放潜力明显增加。土壤水溶性P含量及在酸性条件下P的释放量与土壤总P呈正相关，与土壤pH负相关。     

矿物包裹复合肥的缓释性研究

采用埋土试验法和微区试验方法,对矿物包裹复合肥料的缓释性进行了研究。结果表明,矿物包裹复合肥料的养分释放明显向后期延伸,矿物包裹复合肥料的肥效期可达120 d以上,比复混合肥料的肥效期至少延长80 d,有利于植物均衡吸收养分,其氮的利用效率比等养分复合肥高出38个百分点;其磷的利用效率比等养分复合肥高出11.5个百分点。     

城市生活垃圾的DSC和TGA分析与热值估算

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。     

几种裸子植物胚乳愈伤组织的诱导

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％．     

Simulating the dynamics of sulfur species and zinc in wetland sediments

In situ measurements comparing vertical SO₄²⁻ profiles in vegetated and non-vegetated sediments showed that SO₄²⁻ concentrations in vegetated sediments increased significantly at the beginning of the growing season and then gradually decreased during the rest of the growing season. Throughout the growing season, SO₄²⁻ concentrations remained higher in the vegetated sediments than in the sediments without plants. The higher SO₄²⁻ concentrations in the vegetated sediments indicate that oxygen release from roots and evapotranspiration-induced advection by plants play an important role in the dynamics of sulfur species in sediments. Since the total pool of solid-phase sulfide is relatively large compared to the mass of SO₄²⁻ in the sediments, the gradual decrease of SO₄²⁻ concentrations may result from limitation of the solid-phase sulfide that is in direct contact with or very close to the roots and rhizomes. This would mean that the main pool of solid-phase sulfide and associated trace metals are not affected by the oxygen release from roots, and the associated trace metals will not become bioavailable during the growing season.     

屋顶绿化生态系统箱的研制

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。     

A Numerical and Field Investigation of Surface Heat Fluxes from Small Wind-Sheltered Waterbodies in Semi-Arid Western Australia

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.     

城市热岛效应研究进展

作为现代城市气候主要特征之一的城市热岛效应有日渐严重的趋势。文章综述了城市热岛的生态环境效应、热岛的主要形成机制、时空分布特征等研究状况和发展趋势；基于当前城市热岛研究的现状，提出了未来城市热岛效应研究的方向及缓解城市热岛效应的有关对策。