共查询到20条相似文献,搜索用时 15 毫秒
1.
V. Krishna Prasad K.V.S. Badarinath H. Tsuruta S. Sudo S. Yonemura John Cardina Benjamin Stinner Richard Moore Deborah Stinner Casey Hoy 《The Environmentalist》2003,23(2):175-187
Forests and soils are a major sink of carbon, and land use changes can affect the magnitude of above ground and below ground carbon stores and the net flux of carbon between the land and the atmosphere. Studies on methods for examining the future consequences of changes in patterns of land use change and carbon flux gains importance, as they provide different options for CO2 mitigation strategies. In this study, a simulation approach combining Markov chain processes and carbon pools for forests and soils has been implemented to study the carbon flows over a period of time. Markov chains have been computed by converting the land use change and forestry data of India from 1997 to 1999 into a matrix of conditional probabilities reflecting the changes from one class at time t to another class time t+1. Results from Markov modeling suggested Indian forests as a potential sink for 0.94 Gt carbon, with an increase in dense forest area of about 75.93 Mha and decrease of about 3.4 Mha and 5.0 Mha in open and scrub forests, if similar land use changes that occurred during 1997–1999 would continue. The limiting probabilities suggested 34.27 percent as dense forest, 6.90 as open forest, 0.4 percent mangrove forest, 0.1 percent scrub and 58 percent as non-forest area. Although Indian forests are found to be a potential carbon sink, analysis of results from transition probabilities for different years till 2050 suggests that, the forests will continue to be a source of about 20.59 MtC to the atmosphere. The implications of these results in the context of increasing anthropogenic pressure on open and scrub forests and their contribution to carbon source from land use change and forestry sector are discussed. Some of the mitigation aspects to reduce greenhouse gas emissions from land use change and forestry sector in India are also reviewed in the study. 相似文献
2.
在“3S”技术支持下,利用ASTER卫星图像,建立波段亮度值与植被碳密度间的回归方程,对横断山区西北部的雀儿山西南坡四种植被类型(针叶林、阔叶林、灌木、草)的植被碳贮量进行了估算并分析其影响因素。结果表明,在雀儿山西南坡365.85km2范围内,植被碳贮量共计2.05×106t。区内植被碳密度总体上呈团块状分布,其高值区(125~250t/hm2)主要分布在研究区域北部的俄产至春龙段和南部的金沙江沿岸的格乌、折松渡等地区;中等区域(60~125t/hm2)从北部的俄产至南部的岗托沿色曲河均有分布;而低值区(1~60t/hm2)面积最广,主要分布于北部的贡布堆、上压吧和更庆以南的色曲河河谷内,并在南部的岗托至申龙达段金沙江沿岸形成一个狭长区域。在其影响因素上,不同的植被类型和土地利用方式下碳密度差异较大,而海拔、坡向和坡度对研究区内北部高山亚高山地区植被碳密度影响较南部干旱河谷地区明显。 相似文献
3.
魏国印 《中国环境管理干部学院学报》2001,(1)
地球的碳循环已成为全球气候变化的一个热点,陆地植被是地球破循环中的一个重要贮存库。本文在分析秦皇岛市陆地植被状况的基础上,对CO_2排放量和吸收量进行了估算,结果表明,陆地植被吸收CO_2的数量占排放量的79%。结合秦皇岛市的实际,提出有利于大气碳平衡的对策。 相似文献
4.
Response of Organic and Inorganic Carbon and Nitrogen to Long-Term Grazing of the Shortgrass Steppe 总被引:3,自引:0,他引:3
We investigated the influence of long-term (56 years) grazing on organic and inorganic carbon (C) and nitrogen (N) contents of the plant–soil system (to 90 cm depth) in shortgrass steppe of northeastern Colorado. Grazing treatments included continuous season-long (May–October) grazing by yearling heifers at heavy (60–75% utilization) and light (20–35% utilization) stocking rates, and nongrazed exclosures. The heavy stocking rate resulted in a plant community that was dominated (75% of biomass production) by the C4 grass blue grama (Bouteloua gracilis), whereas excluding livestock grazing increased the production of C3 grasses and prickly pear cactus (Opuntia polycantha). Soil organic C (SOC) and organic N were not significantly different between the light grazing and nongrazed treatments, whereas the heavy grazing treatment was 7.5 Mg ha–1 higher in SOC than the nongrazed treatment. Lower ratios of net mineralized N to total organic N in both grazed compared to nongrazed treatments suggest that long-term grazing decreased the readily mineralizable fraction of soil organic matter. Heavy grazing affected soil inorganic C (SIC) more than the SOC. The heavy grazing treatment was 23.8 Mg ha–1 higher in total soil C (0–90 cm) than the nongrazed treatment, with 68% (16.3 Mg ha–1) attributable to higher SIC, and 32% (7.5 Mg ha–1) to higher SOC. These results emphasize the importance in semiarid and arid ecosystems of including inorganic C in assessments of the mass and distribution of plant–soil C and in evaluations of the impacts of grazing management on C sequestration. 相似文献
5.
Timothy O'Riordan 《Environmental management》1985,9(2):113-119
The British pride themselves on their long tradition of landscape management rooted in the aristocratic and landowning classes of the 18th and 19th centuries. The British also emphasize that the rise of modern pollution control began in the Victorian industrial era with the emergence of the national Inspectorates and the local Commissioners of Sewers. All these traditions are rooted in British social history, which was heavily influenced by class, power, and the changing shape of industrial and agricultural development. In modern Britain, affected by industrial recession, where concern over jobs and growth appears to dominate public and political attention, as well as public spending cuts that sap the morale and effectiveness of the major regulatory agencies, attitudes toward, and the execution of, environmental protection are undergoing a subtle but profound revolution. It is slowly but agonizingly being recognized that economic growth and social well-being cannot be disconnected from environmental processes and the limits these impose on management and technological intervention. A 21st century Britain will have to integrate conservation with development in order to survive. 相似文献
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Naumburg E Mata-Gonzalez R Hunter RG McLendon T Martin DW 《Environmental management》2005,35(6):726-740
Although changes in depth to groundwater occur naturally, anthropogenic alterations may exacerbate these fluctuations and, thus, affect vegetation reliant on groundwater. These effects include changes in physiology, structure, and community dynamics, particularly in arid regions where groundwater can be an important water source for many plants. To properly manage ecosystems subject to changes in depth to groundwater, plant responses to both rising and falling groundwater tables must be understood. However, most research has focused exclusively on riparian ecosystems, ignoring regions where groundwater is available to a wider range of species. Here, we review responses of riparian and other species to changes in groundwater levels in arid environments. Although decreasing water tables often result in plant water stress and reduced live biomass, the converse is not necessarily true for rising water tables. Initially, rising water tables kill flooded roots because most species cannot tolerate the associated low oxygen levels. Thus, flooded plants can also experience water stress. Ultimately, individual species responses to either scenario depend on drought and flooding tolerance and the change in root system size and water uptake capacity. However, additional environmental and biological factors can play important roles in the severity of vegetation response to altered groundwater tables. Using the reviewed information, we created two conceptual models to highlight vegetation dynamics in areas with groundwater fluctuations. These models use flow charts to identify key vegetation and ecosystem properties and their responses to changes in groundwater tables to predict community responses. We then incorporated key concepts from these models into EDYS, a comprehensive ecosystem model, to highlight the potential complexity of predicting community change under different fluctuating groundwater scenarios. Such models provide a valuable tool for managing vegetation and groundwater use in areas where groundwater is important to both plants and humans, particularly in the context of climate change. 相似文献
8.
Recreational use of streams in the Great Smoky Mountains National Park has increased remarkably during recent years. To better manage the stream resource for visitor needs and at the same time preserve it for future generations, a user study was initiated in 1978. Use patterns, both spatial and temporal, and possible accompanying ecological impacts at three streams were investigated. Sampling was conducted at several sites per stream. The findings indicated that use was concentrated during afternoons and at certain streams and study sites. In addition, different types of users partitioned the streams according to stream morphology (form or structure of pools, riffles, etc.). Major impacts observed were soil compaction and erosion along the streambanks and physical disturbance of the stream bottoms by moving and placing stones to construct dams and raceways. 相似文献
9.
四川彭州铜尾矿库植被特征分析与植物群落演替初探 总被引:2,自引:0,他引:2
本文分析了四川彭州铜矿尾矿库的植被特征、群落特征与演替。在该尾矿库上自然定居的高等植物共91种,隶属38科79属,以菊科(Compositae)和禾本科(Gramineae)植物为主。形成6种相对稳定的群落类型;在2003年弃耕后形成的地段分布有史蒿+小飞蓬群落(Artemisia argyi+Conyza conadensis Comm.)、艾蒿+打破碗花花群落(Artemisia argyi+Anemone hupehensis Comm.)、艾蒿群落(Artemisia argyi Comm.)和白车轴苹群落(Trifolium repens Comm.);在经过30~40年自然演替的地段分布有芭茅+羊耳菊群落(Miscanthus sinensis+Inula cappa Comm.)和羊耳菊+千里光+密蒙花群落(Inula cappa+Senecio scandens+Buddleja officinalis Comm.);在近十年内新形成的地段现主要覆盖地衣和葫芦藓(Funaria hygrometrica)。通过对群落结构和不同地段植被特征的对比,对本铜尾矿库的演替现状和规律进行了分析,井讨论了人为影响对演替进程的影响,提出了人工恢复措施的建议。 相似文献
10.
Numerous backcountry and wilderness use studies have been conducted over the last decade, but nearly all of them have concentrated on peak season and summer use. This study investigates use patterns and user characteristics of winter campers, and implications for the management of winter backcountry overnight use. Use pattern data were collected from 580 backcountry use permits for both winter and summer campers of Great Smoky Mountains National Park (GSMNP). A two-page questionnaire was also mailed to 300 of the winter users to survey their characteristics, past backpacking experience, and reasons for winter camping. Backcountry permit data indicate that use patterns differ significantly between winter and summer campers, with winter campers taking shorter, weekend, destination-type trips. Winter campers engage in backcountry camping nearly twice as often during winter as other seasons of the year, both in and outside GSMNP. They are also experienced hikers that tend to avoid camping in Great Smoky Mountains National Park during the summer because of heavy visitor use. This suggests that winter backcountry campers are different enough from peak season campers that management of these two user groups may require different styles. 相似文献
11.
Isolated Spring Wetlands in the Great Basin and Mojave Deserts,USA: Potential Response of Vegetation to Groundwater Withdrawal 总被引:3,自引:0,他引:3
Desert springs, often the sole sources of water for wildlife and cattle, support wetland and wetland/upland transition ecosystems
including rare and endemic species. In the basin and range province in Nevada, USA, springs in the Great Basin and Mojave
deserts are sustained by interconnected deep carbonate and shallow basin-fill aquifers which are threatened by proposed groundwater
withdrawal to sustain rapidly expanding urban areas, a common problem in arid regions worldwide. This paper draws on historic
groundwater data, groundwater modeling, and studies of environmental controls of spring ecosystems to speculate on the potential
effects of groundwater withdrawal and water table decline on spring-supported vegetation. The focus is on springs in the Great
Basin and Mojave deserts representative of those that may be affected by future, planned groundwater withdrawal. Groundwater
withdrawal is expected to reduce spring discharge directly through reduced flows from the shallow basin-fill aquifer or through
reduction of the hydraulic head of the deep carbonate aquifer. This flow reduction will truncate the outflow stream, reducing
the areal cover of wetland and wetland/upland transition vegetation. Lowering the local water table may also reduce the amount
of upland phreatophytic vegetation by causing water levels to drop below plant rooting depths. Percolation of salts to surface
soils may be reduced, eventually altering desert shrub cover from halophytes to nonhalophytes. The extent of these effects
will vary among springs, based on their distance from extraction sites and location relative to regional groundwater flow
paths. On-site monitoring of biotic variables (including cover of selected hygrophytes and phreatophytes) should be a necessary
complement to the planned monitoring of local hydrologic conditions. 相似文献
12.
Many ecological studies use popular variables such as percentage cover of the vegetation to assess the effects of different treatments or environmental management or conditions. Starting with sparse vegetation, the growth in percentage cover is likely to be sigmoidal, and, unless repetitive cover is measured, it will have an upper asymptote of 100%. If the initial cover values under different treatments or management regimes are not equal, then the different growth rates due to the unequal starting values will be confounded with the different treatments.A family of suitable growth curve models can be fitted to the data arising under different treatments, so that one or more of the interpretable fitted parameters of the model can be considered as "responses" to the different treatments. These responses can be analysed to compare the effects of different treatments or environmental conditions, using either parametric or non-parametric methods. The suggested approach is illustrated by application to a particular data set from the literature. The implications for the design of field studies and for the analysis of other vegetational variables are discussed. 相似文献
13.
Changes in vegetation and land use since 1826 were evaluated along the 800 kilometer portion of the Missouri River flood-plain that extends across the State of Missouri using County Land Office Survey records for 1826 and aerial photos for 1937, 1958, and 1972. The combined results show a decline in flood-plain forest coverage from 76% in 1826 to 13% in 1972; cultivated land increased from 18% to 83% during the same time. Uncultivated-unforested areas increased from 6% in 1826 to 27% in 1937, then declined to 1% in 1972; these changes occurred coincident with extensive bank-stabilization and channelization activities initiated in 1912 by the U.S. Army Corps of Engineers. Riverbank stabilization activity since that time may account for the increased rate of decline in flood-plain forests from 0.25% per year between 1826 and 1937 to 1.6% per year between 1937 and 1972.The overall species composition of the 1826 flood-plain forests was found to be most similar to mature forest stands evaluated in 1972; similar frequencies in 1826 and 1972 occurred for hackberry (Celtis occidentalis; 80% in 1826, 83% in 1972), elm (Ulmus spp.; 80% and 83%), and sycamore (Platanus occidentalis; 57% and 50%). Pawpaw (Asimina triloba), found only in mature flood-plain forests in 1972, was recorded along 54% of the 1826 section lines.These combined data indicate (1) that pre-settlement flood-plain forests were extensive and included frequent, mature stands, (2) that in certain areas substantial portions of the flood-plain were in cultivation prior to extensive riverbank stabilization and channelization, and (3) that increased flood-plain forest clearing occurred coincident with increased bank-stabilization activities. 相似文献
14.
Graham Hadley 《Journal of Environmental Planning and Management》1984,27(1):34-38
Enterprise Zones have been in operation as part of government policy for over three years. They contain a special form of planning procedures whereby a general planning permission is given for development subject to certain exclusions and conditions. This article summarises and compares the planning schemes operating in all 25 Enterprise Zones in Britain and considers what have been the results of this planning approach to date in the zones. The operation of these planning schemes has not led to a feared lowering of development standards but nevertheless is not regarded as being suitable for wider application in the planning system. 相似文献
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Timo Karjalainen 《Journal of environmental management》1996,47(4):311-328
The aim of this study was to assess the effects of forest management on carbon sequestration in forests and wood products by using a gap-type forest model interfaced with a wood product model. The assessment is based on total carbon sequestration, i.e. the amount of carbon left in vegetation, litter, soil organic matter and products when the flows of carbon back to the atmosphere have been subtracted. Thirty mixed-species stands, representing medium fertility sites in southern Finland, were included in each simulation for 300 years under current climatic conditions and predicted conditions of changing climate. The average total balance for the first 100 years was higher in the unmanaged system than in the managed system, but for the second and third 100-year periods the results were clearly opposite. Differences in the total balance between the treatments were larger during the first 100 years than over the whole 300-year period. Under conditions of changing climate, differences in carbon sequestration between management options were more pronounced than under current climatic conditions. Under current climatic conditions with the 100-year time frame, the ratio between the total annual balance and annual gross production was 0·208–0·289. Over the whole 300 years, however, efficiency was much lower, 0·088–0·121. Under changing climatic conditions, efficiency was also lower, 0·182–0·252 and 0·081–0·096, respectively. Different management alternatives clearly produced different amounts of timber for the production process; under conditions of changing climate, timber production was substantially enhanced. However, total carbon storages at the end of the simulation varied less than timber production. In the managed system, the flow back into the atmosphere was largest from litter, 41–51% of the total outflow, the flow from vegetation was 23–28%, from soil organic matter 22–25%, emissions from products 1–7%, and emissions from landfills 0–3%. If emissions due to the use of machinery in timber harvesting and transportation were included, they made up only 0·03–0·33% of the total outflow. 相似文献
17.
Soil erosion under different vegetation covers in the Venezuelan Andes 总被引:13,自引:0,他引:13
This comparative study of soil erosion considered different environments in an ecological unit of the Venezuelan Andes. The soils belong to an association of typic palehumults and humic dystrudepts. Soil losses were quantified by using erosion plots in areas covered by four types of vegetation, including both natural and cultivated environments. The highest soil erosion rate evaluated corresponded to horticultural crops in rotation: reaching a value of 22 Mg ha–1 per year. For apple tree (Malus sylvestris Miller) plots, soil losses reached values of 1.96 Mg ha–1 per year. Losses from pasture (Pennisetum clandestinum Hochst. ex Chiov.) plots, without livestock grazing, were as high as 1.11 Mg ha–1 during the second year of the experiment. The highest soil losses generated from plots under natural forest were equal to 0.54 Mg ha–1 per year. Environmental factors such as total and effective rainfall, runoff, and some soil characteristics as those related to soil losses by water erosion were evaluated. The type of management applied to each site under different land use type and the absence of conservation practices explain, to a large extent, the erosive processes and mechanisms. 相似文献
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Loss of grassland species resulting from activities such as off-road vehicle use increases the need for models that predict
effects of anthropogenic disturbance. The relationship of disturbance by military training to plant species richness and composition
on two soils (Foard and Lawton) in a mixed prairie area was investigated. Track cover (cover of vehicle disturbance to the
soil) and soil organic carbon were selected as measures of short- and long-term disturbance, respectively. Soil and vegetation
data, collected in 1-m2 quadrats, were analyzed at three spatial scales (60, 10, and 1 m2). Plant species richness peaked at intermediate levels of soil organic carbon at the 10-m2 and 1-m2 spatial scales on both the Lawton and Foard soils, and at intermediate levels of track cover at all three spatial scales
on the Foard soil. Species composition differed across the disturbance gradient on the Foard soil but not on the Lawton soil.
Disturbance increased total plant species richness on the Foard soil. The authors conclude that disturbance up to intermediate
levels can be used to maintain biodiversity by enriching the plant species pool. 相似文献