湖南省绥宁县黄桑坪自然保护区植物群落多样性分析

通过对湖南省绥宁县黄桑自然保护区的植物群落特征及物种多样性的分析,结果表明:1)可将黄桑自然保护区的滩地、撂荒地和山坡地划分为3种群落类型:鱼腥草-蕨群丛、早熟禾-井栏边草群丛和杉木+马尾松-三尖杉+水苏-莎草+地稔群丛;2)植物多样性指数的大小顺序为:Patrick丰富度指数(R)、Simpson指数(D)和ShannonWiener指数(H)的大小顺序为:山坡地(S,D,H)撂荒地(S,D,H)滩地(S,D,H),Pielou均匀度指数(E)的大小顺序为:潍地(E)撂荒地(E)山坡地(E);3)3种样地之间的物种Czekanowski相似性系数(CC)较低,在0.0001~0.356 8之间,样地内的物种相似性指数(CC)沿滩地→撂荒地→山坡地的顺序递减;(4)相关分析表明:S、D、H之间呈极显著正相关(P0.01),E与S、D、H呈显著负相关(P0.05).生境条件差异是物种多样性差异形成的直接原因.表3,参16.     

土地利用、覆被变化（LUCC）与环境变化关系研究进展

土地利用、覆被变化（LUCC）作为环境变化的主要原因之一,已成为全球变化研究的前沿和热点问题。文章总结了国内外 LUCC 与环境变化关系的主要研究成果和方法,继而从气候、碳循环、土壤环境、水环境以及生态环境对土地利用方式的限制等方面概括了 LUCC 与环境变化之间的关系。LUCC 通过改变大气成分和下垫面性质对气候造成影响;影响着陆地生态系统的碳循环;改变土壤的理化性质,带来土壤污染、土壤养分迁移等土壤质量问题;并且引起水体的非点源污染,影响区域的产水量和水循环。同时,环境变化对LUCC具有限制作用。不仅通过特定的气候环境直接限制土地的利用方式;还间接通过借助人类生态环境意识的改变,实现对区域土地利用强度与方式的约束。LUCC既是全球环境变化的原因,也是全球环境变化的结果。LUCC 与生态环境之间存在着复杂的、非线性的动态反馈关系。进一步探讨了当前 LUCC 与环境变化关系的主要研究方向和相关研究方法,针对目前存在的缺乏统一的指标体系,研究区域、时空尺度单一,以单要素静态研究为主,实验研究相对薄弱以及动态模拟不够等问题,提出加强跨学科综合交叉研究、注重多尺度探讨LUCC的环境效应、构建一个 LUCC 环境效应研究的统一指标体系及加强“3S”技术与模拟模型的融合等建议。为寻求更科学更合理的土地利用方式提供了基础信息。     

Effects of nutrient concentration and litter cover on quantitative shoot parameters and belowground biomass of Zizania latifolia (L)

This study investigated the effect of nutrient concentration and litter cover on the development of quantitative shoot parameters and belowground biomass (BGB) production of Zizania latifolia. Zizania latifolia is a common emergent aquatic species in East Asia. Four treatments were done at the study site, and were observed between May 2003 and December 2005. The treatments are namely, high nutrient (HN) with litter cover (HNWL), high nutrient without litter cover (HNNL), low nutrient (LN) with litter cover (LNWL), and low nutrient without litter cover (LNNL). The quantitative shoot parameters and BGB had higher values for treatments with high nutrient (HN) compared to the low nutrient treatments (LN), independent of the presence of litter cover. Furthermore, the life span of the secondary shoots was also higher in HN treatments compared to LN treatments. The BGB productivity was higher in the HNNL treatment compared to the other treatments. The LNWL treatment showed the least developed quantitative shoot parameters, e.g. plant height, and the lowest BGB for Z. latifolia. It was generally observed that the combined effects of low nutrients and litter cover negatively affected shoot development and BGB production.     

新优草本地被植物在湖南引种初报

该研究在对湖南省及省外草本地被植物应用调查研究的基础上,引进10种草本地被植物,通过观察其在引入地的形态特征、物候期及生态适应性,初步筛选出6种具有推广潜质的品种,即瞿麦、紫娇花、绿苋草、血草、柳叶马鞭草、金叶苔草.旨在为我省基础绿化植物品种的选择提供理论参考,为增添我省植物多样性做出贡献.表3,参5.     

转炉钢渣回收风淬水冷工艺的排风量确定

转炉钢渣回收风淬水冷工艺过程中产生有水蒸气、余热、烟尘等多种工业污染物,工艺排风量确定受到工艺生产过程阵发性、烟气温差大、水蒸气含量多等因素影响。通过研究工艺过程热风平衡,分析确定了工艺过程排风量,其中考虑了分散钢渣液进入排风罩内的压缩空气量、钢渣水冷粒化过程产生的过热水蒸气量以及保证罩内负压的排风量。结合工程实例进行了设计计算。     

Vegetation competition model for water and light limitation. II: Spatial dynamics of groundwater and vegetation

In temperate climates groundwater can have a profound effect on vegetation, because it strongly influences the spatio-temporal distribution of soil moisture in the rootzone and therefore the occurrence of water and oxygen stress of vegetation. This article focuses on vegetation and groundwater dynamics along a hill slope by developing and evaluating a fully coupled hydrological-vegetation model for a temperate forest ecosystem. The vegetation model is described in part 1 of this series of two papers. To simulate the hydrology an extended version of the saturated-unsaturated hydrological model STARWARS has been used. The coupled model is used to investigate both the short and long-term dynamics for a system of two species. Both compete for light and water where one is adapted to wet conditions and the other to dry conditions. The daily dynamics show that the influence of groundwater is particularly strong in spring when waterlogging occurs due to decreased evapotranspiration in winter. Long simulation runs of 1000 years were performed to study the equilibrium state for the two species. Comparison of simulation results with observations of groundwater depth and vegetation types along a dry-wet gradient in a natural forest shows that a reductionist approach is able to capture these patterns well. Sensitivity analysis shows that the border between wet- and dry-adapted species moves upslope with increased rainfall, decreased slope angle and decreased aquifer thickness. These results are similar to previous findings which were based on global maximization of ecosystem evaporation or minimizing ecosystem stress. Comparison of runs with a fixed and a dynamic groundwater table shows that a dynamic groundwater table facilitates a wider transition zone between vegetation types along the hill slope. In this transition the biomass of vegetation is higher in the case of a dynamic groundwater than in case of a static groundwater table. This underlines the importance of incorporating spatial groundwater dynamics in models of groundwater influenced ecosystems.     

Allometric scaling of resource acquisition by ruminants in dynamic and heterogeneous environments

We present a mechanistic formulation of the intake response of ruminants to vegetation biomass based solely on physiological and morphological parameters that scale allometrically with the animal's body mass. The model is applied to describe herbivore-vegetation interactions in dynamic and heterogeneous landscapes with low quality but abundant “tall grass” and high quality but sparsely available “short grass”, under two conditions: “uncoupled” (such that the effect of food intake on vegetation biomass can be neglected), or “coupled” (such that the vegetation biomass is determined by herbivore feeding). The results show that under uncoupled conditions, the minimum acceptance (proportion of vegetation consumed by the herbivore) at which the herbivore can leave its current patch without reducing its intake rate is when it has depleted the current patch by the energetic cost required to travel to another patch. The maximum acceptance at which the herbivore should leave its patch is when it has depleted the current patch by the cumulative energetic cost of traveling, handling, cropping, and digesting. Under coupled conditions, the optimal acceptance equals half the relative growth rate of the vegetation. Analytical solutions are obtained for equilibrium values for utilization of the vegetation, and for the densities of vegetation and ruminants, expressed in physiological and morphological herbivore parameters.     

Climate- and human-induced woody vegetation changes in Botswana and their implications for human adaptation

For purposes of suggesting adaptive and policy options regarding the sustained use of forestry resources in Botswana, an analysis of the whole countrywide satellite data (showing the mean present distribution of vegetation in terms of species abundance and over all density) and the projection of vegetation cover changes using a simulation approach under different climatic scenarios were undertaken. The analysis revealed that changes in vegetation cover types due to human and natural causes have taken place since the first vegetation map was produced in 1971. In the southwest, the changes appear to be more towards an increasing prevalence of thorn trees; in the eastern part of the country where widespread bush encroachment is taking place, the higher population density suggests more human induced (agrarian-degradation) effects, while in the sparsely settled central Kalahari region, changes from tree savanna to shrubs may be indicative of the possible influence of climate with the associated effects of fires and local adaptations. Projection of future vegetation changes to about 2050 indicates degeneration of the major vegetation types due to the expected drying. Based on the projected changes in vegetation, current adaptive and policy arrangements are not adequate and as such a shift from the traditional adaptive approaches to community-based types is suggested. Defining forestry management units and adopting different management plans for the main vegetation stands that are found in Botswana are the major policy options.     

Simulating the impacts of fire: A computer program

Recurrent fire has played a dominant role in the ecology of southwestern ponderosa pine forests. To assess the benefits or losses of fire in these forests, a computer simulation model, called BURN, considers vegetation (mortality, regeneration, and production of herbaceous vegetation), wildlife (populations and habitats), and hydrology (streamflow and water quality). In the formulation of the model, graphical representations (time-trend response curves) of increases or losses (compared to an unburned control) after the occurrence of fire are converted to fixedterm annual ratios, and then annuities for the simulation components. Annuity values higher than 1.0 indicate benefits, while annuity values lower than 1.0 indicate losses. Studies in southwestern ponderosa pine forests utilized in the development of BURN are described briefly.     

Changes in Land Cover and Subsequent Effects on Lower Fraser Basin Ecosystems from 1827 to 1990

/ European settlement began in the Lower Fraser Basin (LFB) inwestern British Columbia in 1827 and has impacted the basin ecosystem in anumber of ways, especially affecting the vegetation. Using previouslypublished data, air photos, and other historical material for the area,estimates of land cover were made for the years prior to 1827 and for 1930and 1990. The area of coniferous forest changed from 71% prior to 1827to 50% in 1930 to 54% in 1990. However, prior to 1827, only27% of the forest would have been immature (<120 years old), while40% would have been immature in 1930 and 73% of the forest wasimmature in 1990. The amount of wetland area decreased from 10% to1% of the study area while urban and agricultural area increased to26% of the study area by 1990. The changes in land cover have hadadverse effects on soil, water, and air quality; aquatic life; and plant andanimal populations. Estimates of changes in net primary production andorganic soil carbon suggest a decline over the past 170 years, although thelatter rate of decrease has slowed since 1930. As human populations in theLower Fraser Basin continue to increase, the quality of air, water, and soilwill continue to decline unless measures are taken.KEY WORDS: Human impact; Land cover; Net primary productivity; Organiccarbon in soil