沂河流域土地利用时空变化图谱特征分析

基于沂河流域1995年、2005年和2015年土地利用空间数据,运用地学信息图谱方法构建1995-2005年和2005-2015年两个时序单元的土地利用转移图谱和涨落势图谱,分析了沂河流域近20年来的土地利用时空变化规律及发展过程。结果表明：（1）1995-2015年,沂河流域土地利用结构以耕地和林地为主,其中耕地和草地减少,林地和建设用地增加是主要变化趋势。（2）土地利用转移图谱以耕地与林地、草地之间的相互转换以及建设用地占用耕地为主,林地、草地转变为耕地主要发生在费县和平邑县中部地势平缓的山前平原,耕地转变为林地、草地则主要分布于研究区北部和西南部土壤侵蚀较为严重的山区,耕地转变为建设用地主要集中在各县市城区周边经济相对发达的区域。两个时序单元中,发生变化的主要图谱单元类型及面积存在显著差异,2005-2015年土地利用发生转换的空间进一步扩张。（3）土地利用涨势图谱中新增耕地面积最大,占新增面积的比例为33.87%;落势图谱中耕地萎缩面积最大,占萎缩面积的比例为51.38%。两个时序单元中,各县市涨落势图谱变化存在明显差异。该研究可为沂河流域土地资源的可持续利用及生态建设提供科学依据。     

Why a 100-Year Time Horizon should be used for GlobalWarming Mitigation Calculations

Global warming mitigation calculationsrequire consistent procedures for handlingtime in order to compare `permanent' gainsfrom energy-sector mitigation options with`impermanent' gains from many forest-sectoroptions. A critical part of carbonaccounting methodologies such as thosebased on `ton-years' (the product of thenumber of tons of carbon times the numberof years that each ton is held out of theatmosphere) is definition of a timehorizon, or the time period over whichcarbon impacts and benefits are considered. Here a case is made for using a timehorizon of 100 years. This choice avoidsdistortions created by much longer timehorizons that would lead to decisionsinconsistent with societal behavior inother spheres; it also avoids a rapidincrease in the implied value of time ifhorizons shorter than 100 years are used.Selection of a time horizon affectsdecisions on financial mechanisms andcarbon credit. Simple adaptations canallow a time horizon to be specified andused to calculate mitigation benefits andat the same time reserve a given percentageof weight in decision making forgenerations beyond the end of the timehorizon. The choice of a time horizon willheavily influence whether mitigationoptions such as avoided deforestation areconsidered viable.     

呼和浩特市地表水水质变化趋势分析

对黄河(过境)、大黑河水系及浑河水系十年水质检测结果进行综合分析,揭示其变化趋势,并针对各河流污染断面提出急需解决的问题.     

Revisit ocean thermal energy conversion system

The earth, covered more than70.8% by the ocean, receives most of itsenergy from the sun. Solar energy istransmitted through the atmosphere andefficiently collected and stored in thesurface layer of the ocean, largely in thetropical zone. Some of the energy isre-emitted to the atmosphere to drive thehydrologic cycle and wind. The wind fieldreturns some of the energy to the ocean inthe form of waves and currents. Themajority of the absorbed solar energy isstored in vertical thermal gradients nearthe surface layer of the ocean, most ofwhich is in the tropical region. Thisthermal energy replenished each day by thesun in the tropical ocean represents atremendous pollution-free energy resourcefor human civilization. Ocean ThermalEnergy Conversion (OTEC) technology refersto a mechanical system that utilizes thenatural temperature gradient that exists inthe tropical ocean between the warm surfacewater and the deep cold water, to generateelectricity and produce other economicallyvaluable by-products. The science andengineering behind OTEC have been studiedin the US since the mid-seventies,supported early by the U.S. Government andlater by State and private industries.There are two general types of OTECdesigns: closed-cycle plants utilize theevaporation of a working fluid, such asammonia or propylene, to drive theturbine-generator, and open-cycle plantsuse steam from evaporated sea water to runthe turbine. Another commonly known design,hybrid plants, is a combination of the two.OTEC requires relatively low operation andmaintenance costs and no fossil fuelconsumption.OTEC system possesses a formidablepotential capacity for renewable energy andoffers a significant elimination ofgreenhouse gases in producing power. Inaddition to electricity and drinking water,an OTEC system can produce many valuableby-products and side-utilizations, such as:hydrogen, air-conditioning, ice,aquaculture, and agriculture, etc. Thepotential of these by-products, especiallydrinking water, aquaculture andmariculture, can easily translate intobillions of dollars in businessopportunities. The current status of theOTEC system definitely deserves to becarefully revisited. This paper willexamine recent major advancements intechnology, evaluate costs andeffectiveness, and assess the overallmarket environment of the OTEC system anddescribe its great renewable energypotential and overall benefits to thenations of the world.     

Bioenergy to mitigate for climate change and meet the needs of society,the economy and the environment

Changes towards environmental improvementsare becoming more politically acceptableglobally, especially in developedcountries. Society is slowly moving towardsseeking more sustainable productionmethods, waste minimisation, reduced airpollution from vehicles, distributed energygeneration, conservation of native forests,and reduction of greenhouse gas (GHG)emissions. Modern biomass, when used tosupply useful bioenergy services, has arole to play in each one of theseenvironmental drivers at both the large andsmall scales.This paper describes recent developments inbiomass supply and the technologies for itsconversion to bioenergy including biofuelsfor transport. It examines the economic,environmental and social benefits andidentifies barriers to bioenergy projectimplementation. Future opportunities forbiomass as a carbon (C) sink, a C offsetand a potential source of renewablehydrogen are discussed.Whether or not a bioenergy project iseconomically viable, as well as being trulyrenewable, sustainable and environmentallysound, is determined mainly by the sourceof biomass. The social benefits from usingbiomass are also valuable, though they areoften not clearly presented when proposingnew bioenergy projects or conductinganalyses of existing plants. Employmentrates per MWh or per GJ exceed those whenusing fossil fuel supplies to provide thesame energy service. `Ownership' bystakeholders and local communities at anearly stage in the development process isthe key to successful project developmentin order to share the benefits. Bioenergyhas a significant global role to play inthe mitigation of atmospheric GHG concentrations.     

Relationships between Danish organic farming and landscape composition

This article presents an investigation of relationships between organic farming and landscape composition in Denmark. Landscape composition was analysed in terms of density of uncultivated landscape elements (I), number of land uses per hectare (II), diversity of land use (III) and mean field size (IV). Two analytical approaches were used. The first was based on an examination of the national agricultural registers for 1998, 2001 and 2004. The second approach used aerial photo interpretation for an analysis of 72 conventional and 40 organic farms within three sample areas for 1982, 1995 and 2002. The national analysis indicated that organic farming has a direct effect on landscape composition. In 2001, organic farms were characterised by a higher number of land uses per ha, a higher land use diversity and smaller mean field sizes. From 1998 to 2004, conversion to organic farming was related to an increasing number of land uses per ha, increasing land-use diversity and decreasing mean field sizes. Relationships between organic farming and landscape composition were independent of variations in regional location, farm size or farm size change. At the level of sample areas, a significant relationship between organic farming and landscape composition was only found for densities of small biotopes. However, when differences in farm size and physical geographical conditions between conventional and organic farms were taken into account, several significant differences in landscape composition were clarified in two of the three sample areas. Furthermore, changes in landscape composition following conversion to organic farming were largely biased by the characteristics of the sample areas. Thus, in contrast to the national level, the sample area study indicated that differences in landscape composition between organic and conventional farms were not a direct implication of organic farming practices, but were related to variations within other parameters and to the location of organically farmed land.     

抚顺市大气降尘污染状况及变化趋势分析

对抚顺市20年来城市环境空气中自然降尘的污染状况及变化趋势进行了全面分析。分析认为抚顺市环境中自然降尘的污染比较重,其中工业区的污染十分严重，交通区的污染也呈上升趋势，近几年由于沙尘天气的频繁出现，导致春季污染加重。并针对降尘的污染状况及变化趋势，提出相应的治理办法及防治途径。     

Prospects for mitigating carbon,conserving biodiversity,and promoting socioeconomic development objectives through the clean development mechanism

Should forest-based climate mitigationmeasures be approved for crediting through the CleanDevelopment Mechanism (CDM), they could offer anopportunity to accomplish three important objectives:cost-effective reductions in carbon emissions andsequestration of atmospheric carbon; conservation andrestoration of forests and their biological diversity;and, the assistance of host countries and communitiesin their socioeconomic development. However,prospective investors in CDM projects, host countriesand other CDM `stakeholders' might be expected toplace widely different priorities on achieving theseobjectives. This paper describes several factors thatwill affect investor interest in CDM projects, thecharacteristics of forest-based CDM projects that willattract investments, and an approach to identifyingprojects that meet the key objectives of multiplestakeholders. This approach entails identifyingsites, such as degraded watersheds, where CDMfinancing for forest conservation and restoration cangenerate readily monetizable local and regionalsocioeconomic benefits, while mitigating carbonemissions in forests with importance for conservingbiodiversity.     

辽东湾海冰漂移的动力要素分析

利用辽东海JZ20－2海域冰期气象、水文和海冰的实测资料和海冰数值模拟结果，对海冰漂移过程中风和流的拖曳力、海冰内力、科氏力和海面倾斜力要素的基本特征进行了分析；采用海冰热力－动力模式对1999年2月3日6：50至2月5日6：50间辽东湾海冰进行了48h数值模拟，对并JZ20-2海域的海冰动力要素进行了对比分析。发现海冰内力、风和流的拖曳力为同一量级，海面倾斜力和科氏力明显较小，其均值的比例关系依次为14．7：18．8：32．6：1．5：1．0；海冰各动力要素相互影响，共同决定了海冰的漂移速度和运动轨迹。     

1973-2018年布喀达坂峰地区前进冰川遥感监测

冰川跃动是冰川动力不稳定性的表现,影响着全球约1%的冰川。基于1973-2018年208景Landsat MSS/TM/ETM+/OLI遥感影像,对布喀达坂峰地区不同时期前进冰川进行遥感识别。结果表明：（1）1973-2018年布喀达坂峰地区共有7条冰川发生过前进,其中冰川末端快速退缩型冰川有3条,冰川末端波动前进型和冰川末端稳定型冰川各有2条。莫诺马哈冰川和5Y542H0020冰川可能为跃动冰川,且前者正处于跃动阶。（2）近45年间布喀达坂峰地区7条冰川共出现过25次前进现象,各条冰川发生前进次数均多于（含）2次;前进冰川发生时间主要集中于2000s（7次）和1970s（6次）。该地区冰川在各月份均发生过前进现象,推断该地区前进冰川属斯瓦尔巴型。布喀达坂峰地区冰川前进无明显规律,大多数冰川两次前进时间间隔为10年左右。（3）布喀达坂峰地区冰川前进可能受热控和水控机理共同作用,单一的气候变化尚难以解释其变化机理。