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31.
中国城镇化过程中村庄土地整理潜力估算   总被引:40,自引:8,他引:40  
该文在理论分析的基础上,创建了一个定量的数学模型来估算村庄土地整理净增加的潜力。估算结果表明,全国平均整理系数2010年为1.42~2.42、2030年为2.27~3.27,分别可净增加耕地面积173.81~296.58万hm2、279.10~401.86万hm2。通过对不同时间和不同生态区的整理系数比较,村庄土地整理潜力具有明显的时空分布规律。在时序上,随着社会经济的发展和城镇化水平的提高,我国农村人口会逐渐减少,整理潜力逐渐增大;在空间上,东部和中部村庄土地  相似文献   
32.
塔里木河下游生态环境对输水的积极响应   总被引:5,自引:4,他引:5  
塔里木河下游是我国西部生态与环境问题最为突出的地区.由于人类不合理的资源开发,导致该地区生态问题日益突出.本文结合塔里木河下游5次生态输水,通过3年对输水后生态环境变化的监测,就塔里木河下游生态环境对输水的积极响应进行了分析.结果显示:(1)生态输水后地下水位在时间上和空间上各有其变化规律,在时间上近河道水位响应快,远河道水位响应慢.在空间上距河道不同距离和不同河段上地下水上升的幅度不同.(2)输水后天然植被的响应主要表现在植被种类和植被盖度的增加上;(3)鉴于输水后生态响应的范围仍然较小,因此输水工程还应该继续进行并适当调整输水的方式.  相似文献   
33.
三工河流域景观格局的形成与环境分异特征   总被引:11,自引:3,他引:11  
景观格局是地貌格局、土壤格局、水资源格局、植物分布格局及生产力格局等的综合。从景观生态学的角度分析了三工河流域景观格局的形成、分布及其环境分异特征 ,讨论了景观格局与环境分异的相互关系 ,最后阐明了三工河流域山地、绿洲和荒漠景观格局的形成及所处的环境特征。  相似文献   
34.
金沙江干热河谷区退化土壤结构的分形特征研究   总被引:25,自引:5,他引:25  
分形理论是近年来兴起的一种新的研究工具。分析结果表明 :土壤粒径分布的分形维数能客观地反映退化土壤的结构状况和退化程度 ,可作为退化土壤结构评价的一项综合性定量指标。退化土壤的分形维数与土壤颗粒组成和微团聚体组成之间存在着明显的相关性。土壤中 <0 .0 0 1mm粘粒含量越高 ,>0 .2 5 mm团粒含量越低 ,则分形维数越高 ,结构性越差。对于同一土壤退化系列 ,分形维数越高 ,土壤退化越严重。  相似文献   
35.
西安草滩渭河古河漫滩沉积与洪水变化   总被引:1,自引:0,他引:1  
根据野外调查、历史文献记录和106个样品的粒度分析,对草滩渭河沉积剖面的洪水变化进行了研究。结果表明,渭河300年来洪水沉积分层明显,对洪水的发生和短期降水量变化反映清楚,分辨率高,能够作为很好地指示洪水和降水量变化的指标。CT剖面厚度约4.5 m,为古洪水沉积层,剖面随深度变化具有明显的粗细变化节律。共分为21个沉积层,指示了21次较大规模的洪水。CT剖面反映的21个阶段的洪水深度和规模由大到小的变化顺序为:第13阶段>第5阶段>第17阶段>第14阶段>第12阶段>第6阶段>第2阶段>第1阶段>第18阶段>第4阶段>第3阶段>第10阶段>第11阶段>第8阶段>第21阶段>第9阶段>第15阶段>第20阶段>第19阶段>第16阶段>第7阶段,其中第13,5,17,14,12,6,2,1阶段为特大洪水阶段,第18,4,3,10,11,8,21,9,15,20,19,16,7阶段为大洪水阶段。CT剖面粒度成分显著大于120年来的洪水沉积,反映了草滩剖面洪水发生时,水动力强,流量大,指示当时降水量应当较多。西安草滩CT剖面第1,2,5,6,12,13,14,17层沉积时,高出河床之上的洪水深度大于6.5 m,其余15个阶段的洪水深度等于或小于6.5 m。  相似文献   
36.
The increasing shortage in water resources is a key factor affecting sustainable socio-economic development in the arid region of Northwest China(ARNC). Water shortages also affect the stability of the region's oasis ecosystem. This paper summarizes the hydrological processes and water cycle of inland river basins in the ARNC, focusing on the following aspects: the spatial-temporal features of water resources(including air water vapor resources, runoff, and glacial meltwater) and their driving forces; the characteristics of streamflow composition in the inland river basins; the characteristics and main controlling factors of baseflow in the inland rivers; and anticipated future changes in hydrological processes and water resources. The results indicate that:(1) although the runoff in most inland rivers in the ARNC showed a significant increasing trend, both the glaciated area and glacial ice reserves have been reduced in the mountains;(2) snow melt and glacier melt are extremely important hydrological processes in the ARNC, especially in the Kunlun and Tianshan mountains;(3) baseflow in the inland rivers of the ARNC is the result of climate change and human activities, with the main driving factors being the reduction in forest area and the over-exploitation and utilization of groundwater in the river basins; and(4) the contradictions among water resources, ecology and economy will further increase in the future. The findings of this study might also help strengthen the ecological, economic and social sustainable development in the study region.  相似文献   
37.
《African Zoology》2013,48(1):295-299
Seed removal from bait stations was studied in miombo habitat in western Zimbabwe. Previous studies of seed predation in southern Africa have largely been conducted in desert ecosystems. However, this woodland-savanna habitat is more mesic and has relatively predictable rainfall patterns. The experiment was conducted in grassy and woody microhabitats in the hot, dry season and early wet season, and followed a year in which precipitation was 69% of the long-term average. Birds removed the greatest quantity of seeds, followed by ants and then rodents. Previous studies in northern hemisphere mesic environments emphasize the importance of rodents and minor role of invertebrates in seed predation. Although our site appears to have more in common with southern hemisphere desert sites than with northern hemisphere mesic sites, we recognize thatour results are likely to reflect a lower limit of consumption by rodents.  相似文献   
38.
The survival of two Atlantic salmon stocks that inhabit rivers confluent with the North Sea was examined in respect to historical distributions of sea surface water temperatures. The rivers Figgjo and North Esk are relatively small salmon rivers in southern Norway and eastern Scotland, respectively. Wild salmon smolts have been tagged in these rivers since 1965. Tag returns were used to evaluate the survival of salmon in the North Sea. Survival rates of one-sea-winter (1SW) and 2SW fish were correlated within stocks, as well as between stocks. Survival rates were compared with the areal extent of thermal habitat in the north-eastern Atlantic Ocean. A positive correlation was found between the area of 8–10°C water in May and the survival of salmon. A reciprocal negative correlation was also found between survival and 5–7°C water in the same month. An analysis of sea surface temperature distributions for periods of good vs. poor salmon survival showed that when cool surface waters dominate the Norwegian coast and North Sea during May, salmon survival has been poor. Conversely, when the 8°C isotherm has extended northward along the Norwegian coast during May, survival has been good. The effect of water temperature distributions on the growth of postsmolts and other survival factors are discussed.  相似文献   
39.
1. The effect of riparian ecotone functional complexity and stream hydraulics on an upland river ecosystem has been analysed. 2. The amount of nutrients retained by bottom sediment was lowest on a sandy substrate (range: 26–104 mg m−2 P-PO4) and highest in wetland bays (range: 558–5368 mg m−2 P-PO4). A stream bed covered by Berula erecta had about three times higher retentive nutrient capacity ( = 584 mg m−2 day−1) than did a sandy substrate( = 205 mg m−2 day−1). 3. The amount of allochthonous organic matter (CPOM) deposited on the stream bed decreased with current velocity. The trophic potential of CPOM, measured as total protein, was significantly correlated with the amount of deposited CPOM (r = 0.863; p<0.00001) and depended on stream order. 4. Both invertebrate and fish biomass in the upland river were significantly correlated with calcium/bicarbonate (benthos: r = 0.858; p<0.006; fish: r = 0.918; p<0.001). 5. Fish biomass, diversity and species richness were highest in pools, lower in riffles and lowest in the run/transition zone. 6. Macroinvertebrate biomass was highest at an intermediate riparian ecotone complexity with an adequate supply of organic matter and incident light. Fish biomass followed the same trend, being lowest in heavily shaded areas and in open channels without riparian vegetation (range: 1–4.5 g m2), but highest in ecotones of intermediate complexity (range: 1.6–92.8 g m2). The ‘cascading effect’ of invertebrate density depletion, which was inversely related to fish biomass, was observed seasonally. 7. The above results indicate that riparian ecotone structure and the heterogeneity of the stream channel may regulate biodiversity, productivity and nutrient retention in the fluvial corridor. These quantitative data help to create alternative scenarios for sustainable river basin management. © 1998 John Wiley & Sons, Ltd.  相似文献   
40.
  • 1. The dispersal ability of species and the geographic scale of habitat fragmentation both may influence the extent of gene flow between fragments, but their interactions have rarely been tested, particularly among co‐occurring species.
  • 2. Population genetic structures of three species of aquatic insect were compared in streams fragmented by reservoirs and in unfragmented streams in north‐eastern Japan, using 52, 37, and 58 RAPD markers. The three species studied included a strong disperser Cincticostella elongatula (Ephemeroptera: Ephemerellidae), an intermediate disperser Stenopsyche marmorata (Trichoptera: Stenopsychidae), and a weak disperser Hydropsyche orientalis (Trichoptera: Hydropsychidae).
  • 3. The patterns of genetic isolation by distance (IBD) supported a priori hypotheses of dispersal ability. The strong disperser (C. elongatula) exhibited significant IBD only at the largest spatial scale studied (among drainages, r=0.50, P<0.01). The intermediate disperser (S. marmorata) showed IBD both within (r=0.22, P<0.01) and among (r=0.45, P<0.01) drainages. The weak disperser (H. orientalis) did not exhibit significant IBD at any scale.
  • 4. Pairwise genetic differentiation (θ) indicated that neither the weak disperser nor the strong disperser were genetically differentiated above and below reservoirs when compared with reference sites. This was in contrast to previous results for S. marmorata, for which subpopulations were genetically fragmented across larger (>4.1 km), but not smaller (<2.9 km) reservoirs.
  • 5. We suggest that intermediate dispersers, i.e. those at equilibrium between migration and genetic drift within drainages, are more likely to be affected by fragmentation than either strong or weak dispersers. Intermediate dispersers could therefore be used as indicator species in studies aimed at detecting the effects of distance between habitat fragments (e.g. reservoir size) for conservation planning. Copyright © 2010 John Wiley & Sons, Ltd.
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