49 resultados para spatial pattern


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We propose a novel communication technique which utilizes a set of mutually distinguishable optical patterns instead of convergent facula to transmit information. The communication capacity is increased by exploiting the optical spatial bandwidth resources. An optimum detector for this communication is proposed based on maximum-likelihood decision. The fundamental rule of designing signal spatial pattern is formulated from analysis of the probability of error decision. Finally, we present a typical electro-optical system scheme of the proposed communication. (c) 2006 Elsevier GmbH. All rights reserved.

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The spatial pattern of the small fish community was studied seasonally in 1996 in the Biandantang Lake. Based on plant cover, the lake was divided into five habitats, arranged in the order by plant structure complexity from complex to simple: Vallisneria spiralis habitat (V habitat), Vallisneria spiralis-Myriophyllum spicatum habitat (V-M habitat), Myriophyllum spicatum habitat (M habitat), Nelunbo nucefera habitat (N habitat), and no vegetation habitat (NV habitat). A modified popnet was used for quantitative sampling of small fishes. A total of 16 fish species were collected; Hypseleotris swinhonis, Ctenogobius giurinus, Pseudorasbora parva, Carassius auratus and Paracheilognathus imberis were the five numerically dominant species. In both summer and autumn, the total density of small fishes was about 10 ind m(-2). Generally, Ctenogobius giurinus, a sedatory, benthic fish, was distributed more or less evenly among the five habitats, while the other four species had lower densities in the N habitat and NV habitat, which had the simplest structures. The distribution of the small fish species showed seasonal variations. In winter, most species concentrated in the V habitat, which had the most complex structure. In spring, the fish had low densities in the N and NV habitat, and were more or less evenly distributed in the other habitats. In summer, the fish had a low density in the NV habitat, and were evenly distributed in the other habitats. In autumn, the fish had higher densities in the V-M and M habitats than in the others. Generally, spatial overlaps between the dominant species were higher in winter than in the other seasons. It was suggested that the variations in the importance of predation risk and resource competition in habitat choice determined the seasonal changes of spatial patterns in the small fishes in the Biandantang Lake.

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It is more and more acknowledged that land-use/cover dynamic change has become a key subject urgently to be dealt with in the study of global environmental change. Supported by the Landsat TM digital images, spatial patterns and temporal variation of land-use change during 1995 -2000 are studied in the paper. According to the land-use dynamic degree model, supported by the 1km GRID data of land-use change and the comprehensive characters of physical, economic and social features, a dynamic regionalization of land-use change is designed to disclose the spatial pattern of land-use change processes. Generally speaking, in the traditional agricultural zones, e.g., Huang-Huai-Hai Plains, Yangtze River Delta and Sichuan Basin, the built-up and residential areas occupy a great proportion of arable land, and in the interlock area of farming and pasturing of northern China and the oases agricultural zones, the reclamation I of arable land is conspicuously driven by changes of production conditions, economic benefits and climatic conditions. The implementation of "returning arable land into woodland or grassland" policies has won initial success in some areas, but it is too early to say that the trend of deforestation has been effectively reversed across China. In this paper, the division of dynamic regionalization of land-use change is designed, for the sake of revealing the temporal and spatial features of land-use change and laying the foundation for the study of regional scale land-use changes. Moreover, an integrated study, including studies of spatial pattern and temporal process of land-use change, is carried out in this paper, which is an interesting try on the comparative studies of spatial pattern on change process and the change process of spatial pattern of land-use change.

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GIMMS NDVI database and geo-statistics were used to depict the spatial distribution and temporal stability of NDVI on the Mongolian Plateau. The results demonstrated that: (1) Regions of interest with high NDVI indices were distributed primarily in forested mountainous regions of the east and the north, areas with low NDVI indices were primarily distributed in the Gobi desert regions of the west and the southwest, and areas with moderate NDVI values were mainly distributed in a middle steppe strap from northwest to southeast. (2) The maximum NDVI values maintained for the past 22 years showed little variation. The average NDVI variance coefficient for the 22-year period was 15.2%. (3) NDVI distribution and vegetation cover showed spatial autocorrelations on a global scale. NDVI patterns from the vegetation cover also demonstrated anisotropy; a higher positive spatial correlation was indicated in a NW-SE direction, which suggested that vegetation cover in a NW-SE direction maintained increased integrity, and vegetation assemblage was mainly distributed in the same specific direction. (4) The NDVI spatial distribution was mainly controlled by structural factors, 88.7% of the total spatial variation was influenced by structural and 11.3% by random factors. And the global autocorrelation distance was 1178 km, and the average vegetation patch length (NW-SE) to width (NE-SW) ratio was approximately 2.4:1.0.

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Land use and land cover change as the core of coupled human-environment systems has become a potential field of land change science (LCS) in the study of global environmental change. Based on remotely sensed data of land use change with a spatial resolution of 1 km x 1 km on national scale among every 5 years, this paper designed a new dynamic regionalization according to the comprehensive characteristics of land use change including regional differentiation, physical, economic, and macro-policy factors as well. Spatial pattern of land use change and its driving forces were investigated in China in the early 21st century. To sum up, land use change pattern of this period was characterized by rapid changes in the whole country. Over the agricultural zones, e.g., Huang-Huai-Hai Plain, the southeast coastal areas and Sichuan Basin, a great proportion of fine arable land were engrossed owing to considerable expansion of the built-up and residential areas, resulting in decrease of paddy land area in southern China. The development of oasis agriculture in Northwest China and the reclamation in Northeast China led to a slight increase in arable land area in northern China. Due to the "Grain for Green" policy, forest area was significantly increased in the middle and western developing regions, where the vegetation coverage was substantially enlarged, likewise. This paper argued the main driving forces as the implementation of the strategy on land use and regional development, such as policies of "Western Development", "Revitalization of Northeast", coupled with rapidly economic development during this period.

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Land-use change is an important aspect of global environment change. It is, in a sense, the direct result of human activities influencing our physical environment. Supported by the dynamic serving system of national resources, including both the environment database and GIS technology, this paper analyzed the land-use change in northeastern China in the past ten years (1990 - 2000). It divides northeastern China into five land-use zones based on the dynamic degree (DD) of land-use: woodland/grassland - arable land conversion zone, dry land - paddy field conversion zone, urban expansion zone, interlocked zone of farming and pasturing, and reclamation and abandoned zone. In the past ten years, land-use change of northeastern China can be generalized as follows: increase of cropland area was obvious, paddy field and dry land increased by 74. 9 and 276. 0 thousand ha respectively; urban area expanded rapidly, area of town and rural residence increased by 76. 8 thousand ha; area of forest and grassland decreased sharply with the amount of 1399. 0 and 1521. 3 thousand ha respectively; area of water body and unused land increased by 148. 4 and 513. 9 thousand ha respectively. Besides a comprehensive analysis of the spatial patterns of land use, this paper also discusses the driving forces in each land-use dynamic zones. The study shows that some key biophysical factors affect conspicuously the conversion of different land- use types. In this paper, the relationships between land- use conversion and DEM, accnmlated temperature(>= 10 degrees C) and precipitation were analysed and represented. We conclude that the land- use changes in northeast China resulted from the change of macro social and economic factors and local physical elements. Rapid population growth and management changes, in some sense, can explain the shaping of woodland/grassland - cropland conversion zone. The conversion from dry land to paddy field in the dry land - paddy field conversion zone, apart from the physical elements change promoting the expansion of paddy field, results from two reasons: one is that the implementation of market-economy in China has given farmers the right to decide what they plant and how they plant their crops, the other factor is originated partially from the change of dietary habit with the social and economic development. The conversion from paddy field to dry land is caused primarily by the shortfall of irrigation water, which in turn is caused by poor water allocation managed by local governments. The shaping of the reclamation and abandoned zone is partially due to the lack of environment protection consciousness among pioneer settlers. The reason for the conversion from grassland to cropland is the relatively higher profits of fanning than that of pasturing in the interlocked zone of farming and pasturing. In northeastern China, the rapid expansion of built-up areas results from two factors: the first is its small number of towns; the second comes from the huge potential for expansion of existing towns and cities. It is noticeable that urban expansion in the northeastern China is characterized by gentle topographic relief and low population density. Physiognomy, transportation and economy exert great influences on the urban expansion.

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With the rapid increase of the number and influence of floating population in China, it is urgently needed to understand the regional types of China's floating population and their spatial characteristics. After reviewing the current methods for identifying regional types of floating population, this paper puts forward a new composite-index identification method and its modification version which is consisted of two indexes of the net migration rate and gross migration rate. Then, the traditional single-index and the new composite-index identification methods are empirically tested to explore their spatial patterns and characteristics by using China's 2000 census data at county level. The results show: (1) The composite-index identification method is much better than traditional single-index method because it can measure the migration direction and scale of floating simultaneously, and in particular it can identify the unique regional types of floating population with large scale of immigration and emigration. (2) The modified composite-index identification method, by using the share of a region's certain type of floating population to the total in China as weights, can effectively correct the over- or under-estimated errors due to the rather large or small total population of a region. (3) The spatial patterns of different regional types of China's floating population are closely related to the regional differentiation of their natural environment, population density and socio-economic development level. The three active regional types of floating population are mainly located in the eastern part of China with lower elevation, more than 800 mm precipitation, rather higher population densities and economic development levels.

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Precipitation is considered to be the primary resource limiting terrestrial biological activity in water-limited regions. Its overriding effect on the production of grassland is complex. In this paper, field data of 48 sites (including temperate meadow steppe,temperate steppe, temperate desert steppe and alpine meadow) were gathered from 31 published papers and monographs to analyze the relationship between above-ground net primary productivity (ANPP) and precipitation by the method of regression analysis. The results indicated that there was a great difference between spatial pattern and temporal pattern by which precipitation influenced grassland ANPP. Mean annual precipitation (MAP) was the main factor determining spatial distribution of grassland ANPP (r~2 = 0.61,P < 0.01); while temporally, no significant relationship was found between the variance of AN PP and inter-annual precipitation for the four types of grassland. However, after dividing annual precipitation into monthly value and taking time lag effect into account, the study found significant relationships between ANPP and precipitation. For the temperate meadow steppe, the key variable determining inter-annual change of ANPP was last August-May precipitation (r~2= 0.47, P = 0.01); for the temperate steppe, the key variable was July precipitation (r~2 = 0.36, P = 0.02); for the temperate desert steppe, the key variable was April-June precipitation (r~2 = 0.51, P <0.01); for the alpine meadow, the key variable was last September-May precipitation (r~2 = 0.29, P < 0.05). In comparison with analogous research, the study demonstrated that the key factor determining inter-annual changes of grassland ANPP was the cumulative precipitation in certain periods of that year or the previous year.

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飞秒激光脉冲通过时空变换技术将时域信息变换到空域,通过空域的处理再返回到时域,是实现飞秒激光脉冲整形、测量和控制的一项重要技术。在应用方面,可产生各种所需要的波形.已广泛应用在飞秒化学、信号处理、安全通信、生物学和医学成像等方面。介绍了飞秒时空变换脉冲整形的几种方法。

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本文主要通过大量的植物群落学调查和植被、环境状况的数量分析,分别从植物区系、森林群落及其主要木本物种、干扰和物种多样性五个方面分析了三峡大老岭地区山地植被景观的空间格局及其与环境因子的关系,结果表明: 1) 植物区系:科的分布区类型以热带性质为主;属一级温带性质明显,北温带、东亚和泛热带诸分布类型突出;区系上属于华中植物区系地区的东部。 2) 在垂直梯度上:种子植物属热带分布诸类的比例自海拔400至800米(~1100米)之间呈上升趋势,然后下降;温带分布的第8、9、10、11类随海拔而上升;地中海-中亚中心分布的第12、13类只见于比较干热的河谷地带;东亚分布和中国特有属在海拔900~1100m和1600~1800m段取得小的峰值;世界分布属的比例随海拔而上升,蕨类植物属则相反。 分别用种子植物属的分布型比列构成,和全部521个属的种类数量,对15个海拔段作聚类分析:前者首先反应了海拔1100~1200m处的划分,与植被干扰状况的垂直分布差异一致;后者强调了海拔900/1000m和1800/1900m 处的分异,可能反映了地带性常绿阔叶林基带/常绿落叶阔叶混交林带,和常绿落叶阔叶林带/落叶阔叶林带的分异。 3) 对本地区森林植被的数量分类结果表明:基本上可以分为中低海拔次生落叶 针阔混交林和中高海拔山地常绿落叶阔混交林两大群。第一群主要包括栓皮栎林-杉木林-马尾松林组(低海拔段)和短柄抱栎林-锥栗林组(中低海拔段)。第二群包括中低海拔沟谷常绿阔叶林组、中海拔段常绿落叶阔叶混交林组和高海拔段米心水青冈林-茅栗林组。 DCCA排序区分了11个群落类型或群落组。采用的7个地貌因子变量中效果显著的可归纳为三组:①海拔,主要反映热量和降水梯度;②坡度和坡位,可能主要反映土壤厚度及其水分和养分状况;③坡向及坡位,反映光照条件。其中植被格局的海拔梯度效应最显著。沿海拔梯度分段分析上述诸因子对植被格局差异影响的垂直分布,表明海拔因子的局部效应在海拔600-800m和1500-1700m段最显著;坡向的效应在海拔1600m以上最突出;坡面、坡位、坡形、坡度等因子的作用在海拔中部最大。对植被格局影响因子的贡献进行定量分离,表明地形对对大老岭森林格局具有强烈的控制作用。 4) 对大老岭森林植被275个主要的木本种类进行TWINSPAN分类,得到16个种组;DCCA排序结果将上述16组合并为8群,两方面都主要反映了沿海拔和坡位+坡向的分化;海拔中部的局部地形差异导致物种组的分化比两端更细致和强烈。 根据物种生活型及其在植物群落中的地位,分6个种组进行排序和环境解释,表明:①尽管低海拔地段受到强烈人为干扰,常绿种类仍显示了数量和性质沿海拔梯度的变化;②珍稀物种在海拔梯度上形成两个相对集中的区段,大致对应于山地常绿落叶阔叶混交林带的上下边缘;③先锋树种在中低海拔的中上坡位富集;④在中、高海拔的中低坡位,落叶的乔木伴生种显示了极大的多样性;⑤为数不多的针叶树种在海拔和局部地形梯度上也有明确分异;⑥它们和落叶的栎(Quercus)、栗(Castanea)、水青冈(Fagus)、鹅耳枥(Carpinus)属物种在大老岭地区不同地形部位的植被中起着主要的建群作用。 具体统计海拔梯度上,常绿和落叶的乔、灌木4类物种分布的种数变化表明:海拔1100m以下人为活动干扰与木本物种多样性呈一致的负相关;海拔1100m以上常绿种减少与与落叶种的增加形成对照;1100~1700m之间是落叶乔木种最丰富的地段,海拔1700m以上四类物种数量急剧下降,与山顶脊附近生境多样性降低、植物群落类型趋同有关。另外,典型亚热带的棕榈和蕉只见于海拔1000m以下;针叶树种以海拔1150m左右为界分成两组。前述4类物种的分布边界在海拔850~1050m和海拔1650~1750m之间形成比较明显的峰值,基本对应着山地常绿落叶阔叶混交林带的上下边缘。 根据海拔分布范围,将样方中出现的558种木本植物按常绿乔/灌种和落叶乔/灌种分别分成5个热量生态类群。统计各自的面分比表明:a. 落叶灌木种的多样性分布重心在海拔梯度上的位置比落叶乔木种高,常绿种则相反,因此灌木和类的分布特征能更好的反映次生环境中的植被-气候关系;b. 在海拔850~1850m的木本物种形成巨大的多样性,仅出现于这一段的物种也很可观;亲缘物种的分化和替代突出,反映其对生物多样性发生和维持的意义重大;c. 亚热带中山地带对落叶种生物多样性的意义远大于常绿种。 5)统计全部群落样方内枯立木、倒伏木、断头木和伐桩四类受干扰木的大小、数量、物种以反映地形对干扰的影响:①枯立木以2~15cm径级个体为主,小径级的树种选择性不强,主要分布在山南坡口上坡位,海拔1800m以上尤多,在陡峭的坡地中部减少;其大径级个体的物种构成和分布格局反映了与生境干旱有关干扰的存在。②倒伏木主要分布在海拔1200~1800m之间坡面中部和顶脊两侧,发生频率与坡度成正比;坡地中部以中、小径级阳性树种为主,山坡顶脊两侧的倒伏木则多为大径级的群落优势种。③断头木主要分布在海拔1200~1700m,和海拔1900m以上。小径级的断头木分布格局接近于枯立木,较大径级的断头木则多与倒伏木的分布相关,断头木中少有典型的阳性树种,主要由林下荫耐种构成。④人为砍伐的伐桩主要为中大径级的植被建群种或优势种个体,在海拔1000m以下,1100-1200m和1600-1800m形成三个峰值,其分布主要与人口密度、生产方式、林木种类以及交通运输便捷程度有关,通常沟谷和山脊线上的伐桩密度较大。大老岭地区人为干扰主要反映在海拔1100m以下,自然干扰的格局在海拔1100m以上才得到反映。 6)在不同取样尺度上,对大老岭地区森林群落各层次α多样性和β多样性的空间格局分析表明:i. 乔木层α多样性在海拔1200-1800m之间取值较高,灌木、草本层α多样性的垂直梯度不显著,但在海拔1200-1800m之间的波动变化较为剧烈,南坡面有最丰富的灌木层多样性而西坡乔木层的物种最丰;从植被整体上,海拔1000m以下物种丰富度较低,1000-1700m之间变化剧烈,1700m以上丰富度水平较高。ii. 海拔1000-2000m之间94个样方中,乔、灌、草三层多种生物多样性指数变化影响因子的大小顺序是:坡位>海拔>坡向>坡面>坡度>坡形。乔、灌、草各层几种多样性指数在多维的地形因子梯度上形成各异的分布格局,反映了山地物种多样性格局控制因子的多样性和多尺度,及局部地形因子对景观尺度上生物多样性空间格局的强烈影响。iii.对海拔1050m和1670m处植被α多样性的变尺度分析表明:随取样尺度增大,低海拔乔木、灌木层α多样性增长速率比高海拔大;后者草本层的多样性增长比较快。海拔1050m处群落各层的α多样性在800m~2尺度上渐近稳定;海拔1670m处,400m~2尺度上各层α多样性指数已基本稳定。 南、北、西坡面β多样性沿海拔梯度大致减少,在海拔1600m以上更明显,在海拔梯度中部变化剧烈。反映不同坡面上群落间异质性水平是:西坡>北坡>南坡。 在对植被、环境上述各个方面的格局特征分析基础上,对三峡地区侵入岩山地类型建立了一个综合的植被景观格局模式。 文章最后就两个景观尺度植被-环境的综合性问题进行了讨论:1)气候、植物区系、植被和物种分布等对老岭以至于三峡地区和亚热带山地常绿落叶阔叶混交林带的位置、宽度的反映;和气候、地形、干扰等因子对这一生态过渡带格局和动态的影响;2)三峡地区生物多样性垂直分布的特征、维持和变化的现代机制,以及保护的重点和策略

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本文对松嫩平原羊草地的群落结构及空间格局进行了分析,主要内容包含以下三个方面: 1、本文第一部分是对碱化草地植物群落分布的空间、环境因子分离。决定碱化草地植物物种在空间分布的因素可以大致分解成4个部分:(1)通过物种的生态位起作用的环境因子;(2)决定物种、群落间竞争激烈程度的空间距离因子;(3)环境和空间因子的交叉或耦合作用;(4)其它未知因子(如生物和随机因子)。本研究在1996年野外实地采样的基础上,运用DCA消势对应分析(Detrended Correspondence Analysis)对群落主要变化趋势及其与土壤环境因子之间的关系进行了分析。运用DCCA消势典范对应分析(Detrended Canonical Correspondence Analysis)对影响松嫩平原碱化草地群落结构季节动态的空间和环境因素进行了定量的分解。结果表明: 在影响群落分布的各因子中,环境因子独立约占40%,而环境一空间耦合因子占35%,空间因子独立约占3%,其它因子约占20%。在诸多因子中,土壤的盐渍化程度在整个生长季起着决定性作用,但土壤水分和氮素的作用因季节而变化。在干旱季节,植物生长的主要制约因子表现为土壤碱化度和土壤水份,而土壤氮素的作用处于次要地位。但在降雨较多、土壤湿润度较大的季节,土壤氮素的影响明显增强,成为仅次于土经度的决定性因素。 2、第二部分对东北松嫩平原碱化草地植物群落空间格局的分形性质进行了分析,分别用边长-面积指数和Korcak指数估计了斑块边界复杂性和斑块面积分布的分形维数。结果表明: 随放牧强度增加,占优势的羊草斑块的相对斑块化加剧,而斑块的边界在中度放牧时最不规则: 在水淹地,占优势的羊草斑块和次优势的碱茅斑块、獐茅斑块的斑块边界复杂性和斑块化程度比未水淹地都低,说明水降低了群落复合体内的异质性: 水淹地优势植物斑块的边长-面积指数和Korcak指数均低于次优势种,但在重度放牧地结果好相反,说明两种样地处于不同的演替阶段; 斑块边界复杂性符合同一尺度规律,在现有的面积范围以内没有尺度转换,而斑块面积分布则存在尺度转换点。对重牧地和水淹地的尺度分析表明,较小尺度上, 群落空间格局的相对斑块化程度较低,说明较小尺度上的空间格局要相对稳定一些,而较大尺度上则相反。可能原因是放牧干扰对大尺度的斑块影响更大。 3、对1989年开始围栏封育的样地10年来的空间格局变化进行时间序列分析,研究恢复演替过程中各个主要斑块类型的分布特征及动态,以及整个样地总体格局在演替系列中的变化。得出如下结果: 羊草是该区植被的优势种,其格局动态为:1989-1993年,羊草斑块总面积增加,斑块数目减少,相对斑块化指数降低,1994年后羊草的空间格局基本稳定。 羊草的斑块面积分布曲线在20平方米左右发生转折,即空间格局在此尺度发生尺度转换。不同尺度上斑块的相对斑块化指数及其在恢复演替中的变化趋势不同:小斑块的相对斑块化指数低,在1989-1993年期间增加,而后降低;大斑块的情况正好相反。说明羊草空间格局的主要变化之一是中等大小斑块的合并和数目减少,羊草斑块生长对格局的影响比斑块合并的影响要小。 獐茅斑块的格局动态为:1989-1994,斑块总面积、斑块数目、最大斑块面积增大,1995年开始降低。相对斑块化程度则先降后增。碱蓬斑块在1989-1993年间的格局动态与羊草正好相反:总面积减少,斑块数目增加,斑块面积大小的变化范围变窄,说明1993年之前,控制碱蓬斑块的主要生态学过程是其他物种的侵入,隔离原来较大的斑块,同时占据某些小斑块。1994年之后,碱蓬斑块的变化比较随机,其格局变化受到其他物种如杂草对策种虎尾草等的影响很大。 样地总体格局的变化为:1991年前,斑块种类和总斑块数目增加,斑块化程度随着增大;1993年后,斑块种类基本稳定下来;1991-1995,斑块化指数降低。在此期间,斑块数目增加,所以斑块化程度降低意味着斑块大小频率分布趋于均匀,大斑块被分裂,小斑块在长大,群落总体空间格局逐渐稳定。总体格局在三个尺度上有不同的自相似规律,这三个尺度分别为:La(a)<=1; 15.5。小尺度上相对斑块化程度低,但年际间变化较中尺度剧烈;中尺度相对斑块化程度变化较为缓,大尺度上,斑块分布一直趋于减少最大的斑块数目。总的变化趋势为,随恢复演替的深入,最大和最小的斑块数目都减少,处于中间尺度的斑块最多。

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本文从物种和景观两个组织水平上研究了气候、土壤、地形等自然环境因子和人类活动因子对生物空间分布格局的影响。基于锡林河流域地理信息系统各环境因子的专题数据,利用空间异质性分析方法研究了锡林河流域环境因子的空间分布格局;基于锡林河流域野外调查数据,运用空间异质性分析方法研究了重要物种的空间分布格局,并采用典范对应分析(Canomc Correspondence Analvsis,CCA)方法分析了物种分布与环境因子的关系:基于锡林河流域地理信息系统各环境因子的专题数据,研究了锡林河流域植被斑块的空间格局特征及其与环境因子的关系,并采用典范对应分析方法分析了植被类型组成与环境因子的关系:基于内蒙古草原生态系统定位研究站放牧样地的样方调查数据.采用空间异质性分析方法,研究了放牧压力对物种空间分布格局的影响:基于多年的卫星遥感数据,采用建模和对比等方法,研究了定居放牧方式下植被状况空间变化规律及植被状况时空变化与人类活动、社会经济发展的关系。通过上述分析,得到的主要结论如下: 1、锡林河流域各个环境因子都具有自己的空间特征尺度,共同形成多尺度等级体系,按特征尺度的大小可以分为如下3个组: ·小尺度组(15km左右):有机暖、全N的较小的特征尺度 ·中尺度组(30~50km):T1,碳酸钙含量.PER、全N和海拔高度的较小的特征尺度 ·大尺度组(100km左右):ANNR,PER、全N和海拔高度的较大的特征尺度多尺度等级的生态学意义是它反映生态变量异质斑块的镶嵌和包含特征,环境因子多尺度等级体系反映共性,具有普遍性:反映生态关系,具有生态学意义。 2、对物种空间异质性的Mantel检验和半方差分析得到了一致的结果产即羊草、糙隐子草和星毛萎菱菜在锡林河流域的空间分布呈现随机特征,而大针茅和冷蒿则表现为十分显著的格局特征。按分布格局的显著程度从大到小排列为冷蒿>大针茅>星毛萎菱菜>糙隐子草>羊草。理论半方差图显示大针茅和冷蒿的空间自相关域分别为30.447公里和30公里。物种空间分布格局是受自然条件、人类活动以及它们自身的生理生态特征综合决定的,物种自身的生理生态特征决定了它们对外界环境变化的适应性反应机制,而自然与人类活动这两种因素在空间的交错配置决定了物种适应性反应的方向和程度,从而综合导致物种空间分布格局的形成。 3、对锡林河流域物种分布与环境因子关系的CCA分析和交叉半方差方法分析显示:1)气候因子(11个指标)、土壤性状因子(3个指标)和地形因子(3个指标)对物种分布的贡献率分别为11.2%、9.5%和11%,三者总和为31.7%。2)各个环境因子对物种分布空间作用方向具有一致性,物种分布与环境因子几乎都在135。和157.5。两个方向上具有相对明显的相关性,从锡林河流域来看,这两个方向反映了气候、土壤以及地形从东南往西北的变化梯度方向。 4、对锡林河流域14个植被景观指数进行的PCA分析表明,锡林河流域植被斑块空间分布的物理特征主要表现在斑块的数目和大小方面,其次是在斑块的多样性方面,并可将它们分为4个组,分别反映锡林河流域植被斑块的不同特征: ·第一组:NP、PRD、LPI、MPS、PSSD和TE,主要反映景观斑块在数量和大小方面的特征; ·第二组:SHDI、SIDI、SHEI和SIEI,主要反映景观斑块的多样性特征; ·第三组:PSCV和[J].主要反映景观斑块之间的相互邻接程度; ·第四组:MSI和AWMSI,主要反映景观斑块的形状特征。 MPS和PSSD两个指数与环境因子无论是在相关系数的性质还是显著程度上都保持了很好的一致性,它们与纬度(LAT)及可能蒸散率(PER)呈极显著的正相关关系,而与经度(LNG)、海拔高度(ALT)、年平均降水量(ANNR)及土壤有机质含量(0RG)呈极显著的负相关关系:平均形状指数(MSI)只与LAT呈显著的正相关关系;多样性指数和扩散毗连指数与任何一个环境因子都没有表现出显著的相关性。 5、锡林河流域植被分布与环境因子的关系CCA排序方法分析表明,气候因子(11个指标)、土壤性状因子(3个指标)和地形因子(3个指标)对植被分布的贡献率分别为19.8%、11.1%和14.5%,三者总和为45.4%。环境因子在植被和物种两个水平上的贡献率表现了相似的特点,自然环境因子不能完全解释植被的空间分布,人类活动的影响应该受到重视。 6、放牧压力对物种空间分布格局的研究表明: ·牧压对温带典型草原物种的空间分布格局有明显的影响。随着牧云的增大,属于原生群落物种的羊草与大针茅空间分布的随机性减小,空间自相关尺度逐渐增大;而对于退化过程中的入侵物种冷蒿和星毛萎菱菜,其空间分布的随机性逐渐增大.空间自相关尺度也呈增大趋势。在牧压胁迫超过一定水平时,冷蒿空间分布的自相关尺度开始下降,而星毛萎菱菜的空间分布格局则表现出强烈的随机性。 ·物种空间格局的变化是反映群落演替过程较为稳定的特征,适用于不同放牧条件下 群落之间的比较。 7、利用遥感数据对人类活动对植被影响的研究表明: ·定居放牧方式下,NDVI随定居点距离的变化格局经历了3个阶段。第一阶段,草场处于原生阶段,NDVI不随距离变化;第二阶段,定居点附近开始局部退化,NDVI随距离增加而增大:第三阶段,退化区域扩大,NDVI不随距离变化。 ·在草场局部退化阶段,NDVI随距离的变化呈对数函数规律,定居点的放牧区具有放牧半径、原生NDVI值、NDVI变化率等特征。根据这些特征、NDVI对数规律以及NDVI与地上生物量的关系可以推测定居点的总载畜量。 ·锡林河流域从87年到85年NDVI值降低最大的区域为流域的中部和南部,这与这一区域人类活动强度以及社会经济发展具有密切关系。