51 resultados para 1995-2003


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2003年园林植物的死亡是众多因素的综合作用:偏低气温造成的冷害;干热风的盛行;土壤水分的严重缺乏;连年的干旱;城市夜间路灯的照射;除雪剂的使用等等。

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对1995年世界景观生态学大会和景观生态学发展的国内外现状进行了思考。当今景观生态学与国际生态学的研究热点(全球变化、生物多样性和持续发展)基本一致,但又有自己的特色,其重点领域包括:①生态空间理论与景观异质性研究;②景观变化模型与未来景观规划;③景观系统分析与GIS应用等。由于经济发展和社会生态意识的不同,使得该学科在各地区间的发展很不平衡。着重就我国的本领域研究状况与国际水平作了比较

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Accurate three-dimensional time-dependent quantum wave packet calculations for the N+OH reaction on the (3)A' potential energy surface [Guadagnini, Schatz, and Walch, J. Chem. Phys. 102, 774 (1995)] have been carried out. The calculations show for the first time that the initial state-selected reaction probabilities are dominated by resonance structures, and the lifetime of the resonance is generally in the subpicosecond time scale. The calculated reaction cross sections indicate that they are a decreasing function of the translational energy, which is in agreement qualitatively with the quasiclassical trajectory calculations. The rate constants obtained from the quantum mechanical calculations are consistent with the quasiclassical trajectory results and the experimental measurements. (C) 2003 American Institute of Physics.

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科尔沁左翼后旗位于科尔沁沙地东部农牧交错带 ,生态环境复杂、脆弱 ,资源、人口和环境的协调发展至关重要 ,其土地承载力状况是协调三者关系的重要依据。本文应用系统动力学原理 ,以 1995年为起始年份建立了系统动力学模型 (SD模型 ) ,包括人口、土地资源、种植业、林业、畜牧业、渔业和消费等 7个子系统。选择 3种人口增长速度和 3种营养水平组成 9种方案 ,通过模型的运行预测了科左后旗未来 5 0年人口的动态变化和最大土地资源承载力 ,并对 1995~ 2 0 0 0年实际的人口发展状况和生态状况进行了讨论。研究显示 ,科左后旗土地承载力 4 6 71~ 74 5 1万人 ,不同的方案达到最大承载力的时间不同 ,指出控制人口增长是实现经济环境协调发展的必要条件 ,科左后旗的实际人口增长控制较好 ,现有的环境问题是不合理的开发活动造成的

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通过对自1995-1998年4年的田间及微区试验结果进行总结统计,阐述了松嫩平原春玉米带土壤水分利用率的变化特性及其相应的影响因素,阐述了气候、种植方式、管理水平、土壤肥力及区域与品种类型间对玉米带水分利用率的影响趋势及特性,以期对这一区域的玉米种植提供指导性参考依据。

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KJ85-06项目是“八五”期间由中国科学院资助的最大的生态学研究计划.19个研究所、20个试验站、530余名科技人员参加了该项计划,5年总经费1000万元.研究工作取得了重大进展,迄今已发表论文450余篇、专著3部,尚有大量论文与多部专著将陆续出版.本文简要介绍了有关主要研究进展,并就生态系统优化管理研究和生态过程、人类活动影响联网研究提出了两点主张.

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1995年首次在西藏日喀则进行固沙植物的引种试验,大多数中国内地固沙植物不适应该地的流动沙丘,沙面高温和生长季短是主要制约因素。沙木蓼和籽蒿表现最好;油蒿种子不能成熟,因此不能做后续植物;乡土植物砂生槐在播种当年出苗率低、生长缓慢,只能用做后期植物。在西藏日喀则,有效的植物固沙程序是:在保护措施(草方格沙障、砾石层)下,在流动沙丘上播种外来种沙木蓼、籽蒿和油蒿或移栽籽蒿,同时播种乡土植物砂生槐。在沙木蓼和籽蒿种群衰退、油蒿种群未衰退但不能靠天然下种自行更新时,砂生槐开始发挥固沙作用,并最终凭其适沙特性和长寿命接替先锋固沙植物有效地固定沙丘。选择乡土固沙植物应将重点放在蒿属和锦鸡儿属上。

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运用已建立的EPPML生物地球化学循环模型,对1995年长白山自然保护区生态系统的碳平衡状况进行了模拟.模拟结果表明,该保护区植被的年净初级生产力[NPP(碳量)]为1332×106t·a-1,以阔叶红松林和云冷杉林最高,分别为0540×106t·a-1和0428×106t·a-1.这2种林型是长白山面积最大、生产力最高的林型,其生产力的模拟结果对整个保护区的碳循环和碳平衡影响最大,前者的准确性决定了后者的可靠性.总的来说,模拟值不仅在整个保护区不同植被带和气候带的相对比较中是符合常规的,而且在与相当分散

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对长白山自然保护区的净初级生产力(NPP)的空间分布格局进行了模拟,对它们与环境因子和植被因子间的相互关系进行了分析.结果表明,1995年NPP的模拟值平均为0.680kgC·m-2·年-1,变幅为0.105~1.241kgC·m-2·年-1(82.1%),其中阔叶红松林的NPP最高(1.084kgC·m-2·年-1).环境条件决定了长白山植被年NPP空间分布的大趋势.土壤含水量对NPP的限制最大,呈负相关关系(R=-0.65),长白山植物生长一般不存在水分不足的问题.植被的NPP与LAI高度正相关(R=

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运用已建立的景观尺度生态系统生产力过程模型EPPML对长白山自然保护区地表径流量的季节动态和空间分布特征进行了模拟,对其与环境因子间的相互关系进行了分析.模拟结果表明,长白山自然保护区地表径流量的季节进程表现出明显的三峰型,6月和9月出现低谷,8月达最大(2.58mm·d-1),与土壤含水量的季节变化趋势十分相似.1995年地表径流量的模拟值平均为0.203m·年-1,空间分布随海拔升高呈现明显增加的趋势,最高为高山流砾滩(0.619m·年-1),最低为阔叶红松林(0.081m·年-1).年地表径流量与叶

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描述了一个反映系统碳循环和水循环的景观尺度生态系统生产力过程模型(EPPML).该模型以遥感图像作为数据源,从中获取影响植被生产力的重要变量———叶面积指数(LAI);主要对景观尺度生态系统的净初级生产力(NPP)和蒸散量的空间分布格局和时间动态进行模拟;用地理信息系统(GIS)手段对空间数据进行处理、分析和显示,从而实现将植物生理生态研究的结果从小尺度向中尺度进行拓展和转换.本研究用EPPML对1995年长白山自然保护区的植被生产力进行了模拟,结果表明,EPPML可以比较准确地模拟该保护区主要植被的NP

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The large uncertainties in estimates of cropland area in China may have significant implications for major cross-cutting themes of global environmental change-food production and trade, water resources, and the carbon and nitrogen cycles. Many earlier studies have indicated significant under-reporting of cropland area in China from official agricultural census statistics datasets. Space-borne remote sensing analyses provide an alternative and independent approach for estimating cropland area in China. In this study, we report estimates of cropland area from the National Land Cover Dataset (NLCD-96) at the 1:100,000 scale, which was generated by a multi-year National Land Cover Project in China through visual interpretation and digitization of Landsat TM images acquired mostly in 1995 and 1996. We compared the NLCD-96 dataset to another land cover dataset at I-km spatial resolution (the IGBP DIScover dataset version 2.0), which was generated from monthly Advanced Very High Resolution Radiometer (AVHRR)-derived Normalized Difference Vegetation Index (NDVI) from April, 1992 to March, 1993. The data comparison highlighted the limitation and uncertainty of cropland area estimates from the DIScover dataset. (C) 2003 Elsevier Science B.V. All rights reserved.

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Direct current observations in the Yellow Sea interior are very scarce due to intense fishing and trawling activities. Most previous studies on tides in the area were based on coastal measurements or satellite altimeter sea levels and have not been rigorously compared with direct measurements. In this paper, tidal currents are studied with current profiles from three bottom-moored Sontek Acoustic Doppler Profilers (ADPs) deployed in the southern Yellow Sea in summer of 2001 and 2003. The measured current series were dominated by tidal currents. Maximum velocities are between 40-80 cm/s at the mooring stations. M-2 current is the most dominant primary tidal constituent, while MS4 and M-4 are the most significant shallow water tides with much smaller amplitudes than the primary tides.