耕地不同产量水平的面积与分布监测法

查清中低产田的面积、分布与开发条件是制定农业综台开发规划的重要依据。采用按公里网布设的农业资源动态监测系统,开展对耕地不同产量水平的面积与分布的动态监测,其方法具有准确、简便和实用的特点。     

全新世青藏高原东部西南季风的演变

本研究报道一组新的西南季风代用指标,即泥炭中单一种属植物———木里苔草残体纤维素和泥炭混合植物残体纤维素的δ13C时间序列,所记录的青藏高原东部全新世气候变化。两记录表明,该区全新世的下限年龄约11200aBP(14C年龄约9900aBP);从约11200aBP起该区迅速进入湿暖的全新世阶段,季风活动迅速增强;在约10800～5500aBP期间,季风总体保持在强盛状态,但其间有4次突然减弱,气候变干冷;约从5500aBP起季风活动在波动中逐渐减弱,其中有4次减弱最明显。所有这8次气候的突然变化都与北大西洋浮冰事件一一对应。这种密切的相关关系表明,西南季风强度的波动可能是对全球变化,特别是对海洋热盐环流引起的地球南北方气候波动的所谓"跷跷板效应"的响应。     

铊的水地球化学及环境影响

铊(Tl)是一个典型的毒害金属元素,其对哺乳动物的毒性高于Hg、Cd、Cu、Pb、Zn等元素。Tl在自然水体中存在两种氧化状态:Tl+和Tl3+,通常主要以Tl+形式存在。Tl+易随地下水或地表水的流动而迁移到更远的距离,但在较强的氧化环境中,Tl+能够氧化成Tl3+形成Tl(OH)3的沉淀,可以制约水环境中Tl的总含量。Tl可以通过饮用水进入人体,其中Tl+在人体的酶化反应过程中可以置换K+,并与酶产生很强的亲和力,从而诱发Tl的毒害效应。活性铝净化法、离子交换法和NaCl溶液可以用来去除饮用水中的Tl。基于Tl的毒害性,Tl所产生的水环境问题应该引起重视。     

影响街区峡谷浓度扩散的因素

对街区峡谷内污染扩散规律的研究是城市空气质量预测的主要内容之一。应用现代流体力学数值模拟方法进行大量算例的计算和分析,研究了城市街区峡谷污染物二维扩散的规律。在分析二维街区峡谷内浓度扩散的规律时,发现对街区峡谷浓度扩散的两个影响因素,其中定量分析了湍流脉动对浓度扩散的影响,与层流时得到的浓度扩散进行了通量积分的比较;此外,定性分析了不同类型的街区峡谷对扩散的影响。     

VR-GIS技术在小城镇洪水淹没模拟分析中的应用

近年来利用计算机和信息技术研究洪水灾害是个研究热点,但小城镇在防洪减灾方面缺少应有的关注和重视。本文对VR(虚拟现实技术)-GIS技术在小城镇洪水淹没模拟分析中的应用进行了研究,解决了系统实现过程中的一系列关键技术:小城镇空间数据库的建库技术及三维可视化、洪水淹没范围的确定,以及洪水淹没实时动态演示等问题。该技术已在国家十五科技攻关项目所开发的《小城镇基础设施防灾减灾决策支持系统》中得以实现。实践证明:小城镇空间数据库的建库技术速度快、成本低,适合中国小城镇的信息化现状。利用淹没范围的近似计算模型,可以有效迅速准确地计算出洪水淹没范围,有利于防洪减灾的迅速决策,且偏于安全。小城镇洪水灾害的三维可视化模拟,可以实时动态地演示小城镇遭受洪灾实况的全过程。     

考虑过渡区影响的粉喷桩复合地基承载特性的有限元数值分析

粉喷桩成桩过程中不可避免地会带动桩间土产生强烈的挤压和振动,在固化剂与桩体发生物理化学反应的同时,桩周一定范围内的土体也进行了固化和挤密,使得在桩土交界处形成环向变化的过渡区,过渡区的材料由桩逐渐过渡到桩间土,因此有必要考虑该过渡区对粉喷桩复合地基承载特性的影响。本文从粉喷桩复合地基桩土交界处的特点出发,考虑了桩土材料性质变化的过渡区单元,利用上的摩尔—库仑本构模型,和Plaxis专业岩土软件对粉喷桩复合地基进行了有限元数值分析,就粉喷桩复合地基中桩和土的承载特性得出了一些有益的结论。     

Water quality and health in northern Canada: stored drinking water and acute gastrointestinal illness in Labrador Inuit

One of the highest self-reported incidence rates of acute gastrointestinal illness (AGI) in the global peer-reviewed literature occurs in Inuit communities in the Canadian Arctic. This high incidence of illness could be due, in part, to the consumption of contaminated water, as many northern communities face challenges related to the quality of municipal drinking water. Furthermore, many Inuit store drinking water in containers in the home, which could increase the risk of contamination between source and point-of-use (i.e., water recontamination during storage). To examine this risk, this research characterized drinking water collection and storage practices, identified potential risk factors for water contamination between source and point-of-use, and examined possible associations between drinking water contamination and self-reported AGI in the Inuit community of Rigolet, Canada. The study included a cross-sectional census survey that captured data on types of drinking water used, household practices related to drinking water (e.g., how it was collected and stored), physical characteristics of water storage containers, and self-reported AGI. Additionally, water samples were collected from all identified drinking water containers in homes and analyzed for presence of Escherichia coli and total coliforms. Despite municipally treated tap water being available in all homes, 77.6% of households had alternative sources of drinking water stored in containers, and of these containers, 25.2% tested positive for total coliforms. The use of transfer devices and water dippers (i.e., smaller bowls or measuring cups) for the collection and retrieval of water from containers were both significantly associated with increased odds of total coliform presence in stored water (OR_{transfer device} = 3.4, 95% CI 1.2–11.7; OR_dipper = 13.4, 95% CI 3.8–47.1). Twenty-eight-day period prevalence of self-reported AGI during the month before the survey was 17.2% (95% CI 13.0–22.5), which yielded an annual incidence rate of 2.4 cases per person per year (95% CI 1.8–3.1); no water-related risk factors were significantly associated with AGI. Considering the high prevalence of, and risk factors associated with, indicator bacteria in drinking water stored in containers, potential exposure to waterborne pathogens may be minimized through interventions at the household level.     

黄土区陡坡侵蚀过程试验研究

通过室内放水冲刷试验,结果表明,陡坡单宽径流能耗与单宽径流产沙率之间存在以下线性关系:Dr=18.672(ΔE - 0.751),说明土壤的可蚀性参数为18.672 g/J,发生坡面细沟侵蚀的临界径流能耗为0.751 J/(ms)。坡面单宽径流能耗随流量增大而增加,随坡度变化呈抛物线趋势,临界坡度出现在21和24之间。坡面上各段面单宽径流能耗均随流量的增大而增加,随着坡度逐渐增加,坡面上部段面能耗渐增,中部段面渐减,下部较稳定。坡面各段面侵蚀产沙也有类似特征。此研究对于深入了解黄土高原陡坡土壤侵蚀过程和机理具有重要意义。     

珠江流域土壤中碳库的存量与通量

通过对珠江流域各主要环境介质中不同形态碳含量的分析和计算,得出该流域0~1.0m范围内土壤碳库的存量为1.36×1013kg,占中国陆地碳库总量的9.51%,全球碳库总量的0.907%;流域净碳输入量为4.141×1010kg/a,碳通量912.74kg/(hm2·a),初步计算表明珠江流域可能是陆地生态系统的一个碳汇区。另一方面,人类活动造成流域内有机碳的大量流失,其中,水土流失损失的碳8.01×109kg/a,植物收割及森林砍伐从土壤-植物系统中携带出的有机碳高达6.26×1011kg/a,这将造成土壤有机质含量的降低,因此促进陆地生态系统有机碳存储是提高本流域土地质量的关键。