不同利用方式对江西省农田土壤碳氮磷生态化学计量特征的影响

根据江西省2013年采集的16582个农田耕层(0～20 cm)土壤样点数据,运用实地调查、经典统计学与地统计学等相结合方法,研究了江西省耕地土壤碳氮磷生态化学计量特征的空间变异性及不同农田利用方式对其的影响.研究结果表明:江西省耕地土壤有机碳(SOC)、全氮(TN)和全磷(TP)平均含量分别为17.90、1.58和0.52 g·kg~(-1),土壤碳氮比(C∶N)、碳磷比(C∶P)和氮磷比(N∶P)平均值分别为11.72、38.29和3.38,土壤C∶N∶P比平均值为34.44∶3.03∶1,说明P是江西省耕地土壤主要的限制因素.此外,由于碳、氮、磷三者之间并不存在显著的两两相关性,表明江西省耕地土壤中不存在稳定的"Redfield ratio";半方差函数表明,江西省土壤碳、氮、磷生态化学计量特征具有中等程度的空间变异性,其空间变异特征主要受到随机性因素的影响;经ANOVA检验显示,不同农田利用方式对土壤碳氮磷生态化学计量特征影响显著(p0.05),土壤SOC和TN平均含量依次表现为:两季水田水旱轮作一季水田一季旱地两季旱地,土壤TP平均含量依次表现为:两季旱地两季水田一季水田一季旱地水旱轮作,土壤C∶N依次表现为:两季水田两季旱地一季水田水旱轮作一季旱地,土壤C∶P平均值依次表现为:水旱轮作两季水田一季水田一季旱地两季旱地,土壤N∶P平均值依次表现为:水旱轮作一季旱地两季水田一季水田两季旱地.总体而言,土壤碳、氮、磷生态化学计量比的变化特征是农田利用方式和环境因子综合作用的结果,土壤C∶N∶P比对土壤碳、氮、磷储量及养分的限制性具有重要的指示作用.     

The relationships between awareness of consequences,environmental concern,and value orientations

Different people become engaged in environmental issues and perform proenvironmental behavior because they believe in and are concerned about adverse consequences of environmental problems for themselves (egoistic beliefs and concerns), others (social-altruistic beliefs and concerns), or the biosphere (biospheric beliefs and concerns). These different beliefs and concerns are assumed to derive from corresponding value orientations. Yet, distinguishing egoistic, social-altruistic, and biospheric value orientations has proved difficult in previous research. Based on a survey of 494 Swedish residents between 18 and 69 years old, the present study provides empirical support for that egoistic, social-altruistic, and biospheric environmental concerns are related to corresponding awareness-of-consequences beliefs, and that both the beliefs and environmental concerns are related to the three value types power, benevolence, and universalism.     

青海省的主要灾害类型与防灾减灾对策

论述了青海地区常见的主要灾害类型及危害,并提出了防灾减灾的对策。     

洪水灾害的遥感监测分析系统研究

给出了洪水灾害的遥感监测分析系统,该系统利用遥感信息资料,应用遥感图像处理软件为主要工具,辅助地理信息,分析洪水水情,确定洪灾量级、危害区域及其土地利用类型等,并可比较真实地再现洪灾场景,为防洪规划提供可靠的辅助决策依据。     

生存空间相对性的再研究

生存空间可分为狭义和广义两种,狭义生存空间的特点是有限性和潜在性,扩展性或相对性则是广义生存空间的最大特征;对生存空间的分类研究,有助于某一国家或地区生存现状和发展潜力的评价;人们通过贸易,交换着各自的生存空间;发展经济和科学技术,合理分配生活和生产空间,保护环境,控制人口,以及对资源的合理分配,是人类保护和扩大生存空间努力的基本方面。     

黄土高原半干旱区侧柏林群落土壤呼吸日变化及季节动态变化特征

Desertification is one of the most serious eco-environmental problems around Qinghai Lake. Based on GIS and RS, GIS analysis was used to obtain the information of spatial-temporal change and different pattern of desertification in each county around Qinghai Lake in four phases of 1976, 1987, 1995 and 2006. Using the function of intersect and overlay supported by ARCGIS, with analyzing attributes of vector RS images, we obtained transition data and established transfer matrix of land-use types in recent 30 years, besides, protracted land-use transition maps of all desertification classes. In further, we analyzed transition quantity and direction of desertification in each county, moreover, reconstructed the process of spatial-temporal evolution of desertification. The results are showed below: (1) it′s the transition between desertified land and others but not in the desertified that played the main role in Gangcha and Gonghe County, while the transfer between desertified lands were greater than that with other land-use types in Haiyan County. (2) Extremely severe desertified land mainly distributes in Ketu and Sand Islands that belongs to Haiyan County, and moderate desertified land in riversides of Gangcha County, also, the light desertification expanded too rapidly to become the most desertified land-use type in the surrounding of Qinghai Lake since 1976. (3) By using relative change rate of desertified land, the regional variability rank from top to toe was Gangcha, Haiyan and Gonghe.     

GIS支持下的小尺度土地驱动力研究--以宜兴市湖滏小流域为例

为了能够建立土地演化的模拟模型，在ARCINFO中的GRID模块的支持下，对宜兴市湖滏小流域的土地驱动力进行了探讨，建立了以像元为单位的属性数据库，并随机选取了600个样点。分析则采用了LOGISTIC模型，探讨了社会经济因子与土地类型转移概率间的关系，揭示了任意两个土地类型相互转换的驱动力及整个地区的土地变化驱动力。最后讨论了该模型模拟预测时的局限性，说明其不是合适的模拟模型，而仅是分析土地驱动力较好工具。这种分析是进一步用概率方式逐个模拟地块(patch)演化的基础，因而具有一定的现实意义。     

近10年来长江下游地区耕地动态变化特征

基于遥感资料和GIS分析,对1988～1998年长江下游地区耕地与其他土地利用类型之间相互转变数量特征,以及耕地变化强度、耕地流失强度的区域分异特征进行了分析和描述,对耕地变化导致的环境效应进行了初步探讨。研究结果表明:①1988～1998年,耕地与林地、灌丛、水体之间的转变,对其数量动态变化起着主要作用,在上述转变过程中,耕地总体表现出数量明显减少、质量降低的趋势;②农田向城镇的单向转移,体现了区域快速城市化对耕地的侵占过程,从空间分布看,该过程主要体现于上海、苏锡常地区、南京、杭州等城市化过程最为剧烈的地区;③长江下游地区1988～1998年耕地年均流失率为0.77%,流失的主体部分是位于长江三角洲和巢湖平原自然条件优越、水利灌溉配套设施完善的传统优质耕地,新形成的部分则主要来自于滩涂湿地开垦及低山丘陵地区毁林开荒。总体而言,长江下游地区耕地流失体现在数量锐减、质量下降两个方面,并伴随着一系列生态破坏问题的出现。     

澄江尖山河小流域不同土地利用类型地表径流氮、磷的流失特征

根据径流小区观测, 对澄江尖山河小流域不同土地利用类型地表径流中氮、磷的流失特征进行了研究. 结果表明:灌草丛和次生林都有较好的调节径流和减少土壤流失的作用,在相同的降水量下,坡耕地总产流量分别是人工林、次生林、灌草丛的1.58,12.45和5.52倍;而从产沙量来看,坡耕地的产沙量也远大于其余几种土地利用类型,坡耕地的总产沙量分别是人工林、次生林和灌草丛的8.41,53.06和41.90倍. 不同土地利用类型径流中的总氮、总磷的输出量差异显著,总氮、总磷输出趋势都表现为坡耕地＞人工林＞灌草丛＞次生林;不同土地利用类型径流小区侵蚀泥沙中的总氮、总磷输出量同样为坡耕地＞人工林＞灌草丛＞次生林,且坡耕地的输出量远大于其余几种土地利用类型. 相关分析表明,径流中带走的总氮量大于泥沙,磷的输出主要是以泥沙结合态为主,泥沙是磷的主要载体.      

Contamination by Cd, Cu, Pb, and Zn in mine wastes from abandoned metal mines classified as mineralization types in Korea

The objective of this study was to investigate heavy metal contamination and geochemical characteristics of mine wastes, including tailings, from 38 abandoned mines classified as five mineralization types. Mine waste materials including tailings and soils were sampled from the mines and the physical and chemical characteristics of the samples were analyzed. The particle size of tailings was in the range of 10–100 μm. The pH of the waste covered a wide range, from 1.73 to 8.11, and was influenced by associated minerals and elevated levels of Cd, Cu, Pb, and Zn, extracted by a Korean Standard Method (digestion with 0.1 mol L⁻¹ HCl), which were found in the wastes. Half of the samples contained heavy metals at levels above those stipulated by the Soil Environmental Conservation Act (SECA) in Korea. In addition, extremely high concentrations of the metals were also found in mine wastes extracted by aqua regia, especially those from mines associated with sulfide minerals. Thus, it can be expected that trace elements in mine wastes may be dispersed both downstream and downslope through water and wind. Eventually they may pose a potential health risk to residents in the vicinity of the mine. It is necessary to control mine wastes by using a proper method for their reclamation, such as neutralization of the mine wastes using a fine-grained limestone.