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991.
In a river, the flow directly affects the physical and chemical properties of its water, with further consequences for aquatic
biota. Land use practices and vegetation cover play a significant role in the water cycle. The wide-spread perception of forest
cover, in terms of hydrology is that forests may reduce water runoff: although in rare instances the contrary has been reported.
Water runoff varies seasonally and depends on the forest tree species. By no means can it be considered constant over large
expanses of area or for various rainfall patterns. In this paper, the results of a long-term hydrological survey conducted
in two experimental microbasins (operated by the Institute of Hydrology SAS, IH SAS) with different land use practices are
presented. The Rybárik microbasin (0.119 km2) is dominated by row crop production. The basin was 70% cultivated by the state farm and 30% by a private farm. The Lesny
microbasin (0.086 km2) is covered by a deciduous hornbeam regrowth forest (Carpinus betulus). The analysis revealed that the difference in the
runoff from the forest and the agricultural land increases with increasing precipitation; however, at some point (extreme
precipitations with low probability) the runoff from these basins is nearly equal. 相似文献
992.
The effects of land use and climate change on the carbon cycle of Europe over the past 500 years 总被引:1,自引:0,他引:1
The long residence time of carbon in forests and soils means that both the current state and future behavior of the terrestrial biosphere are influenced by past variability in climate and anthropogenic land use. Over the last half‐millennium, European terrestrial ecosystems were affected by the cool temperatures of the Little Ice Age, rising CO2 concentrations, and human induced deforestation and land abandonment. To quantify the importance of these processes, we performed a series of simulations with the LPJ dynamic vegetation model driven by reconstructed climate, land use, and CO2 concentrations. Although land use change was the major control on the carbon inventory of Europe over the last 500 years, the current state of the terrestrial biosphere is largely controlled by land use change during the past century. Between 1500 and 2000, climate variability led to temporary sequestration events of up to 3 Pg, whereas increasing atmospheric CO2 concentrations during the 20th century led to an increase in carbon storage of up to 15 Pg. Anthropogenic land use caused between 25 Pg of carbon emissions and 5 Pg of uptake over the same time period, depending on the historical and spatial pattern of past land use and the timing of the reversal from deforestation to afforestation during the last two centuries. None of the currently existing anthropogenic land use change datasets adequately capture the timing of the forest transition in most European countries as recorded in historical observations. Despite considerable uncertainty, our scenarios indicate that with limited management, extant European forests have the potential to absorb between 5 and 12 Pg of carbon at the present day. 相似文献
993.
Lamia Miri Guillaume Bouvier Anass Kettani Afaf Mikou Lahcen Wakrim Michael Nilges Thérèse E. Malliavin 《Proteins》2014,82(3):466-478
The HIV‐1 integrase is an attractive target for the therapeutics development against AIDS, as no host homologue of this protein has been identified. The integrase strand transfer inhibitors (INSTIs), including raltegravir, specifically target the second catalytic step of the integration process by binding to the DDE motif of the catalytic site and coordinating Mg2+ ions. Recent X‐ray crystallographic structures of the integrase/DNA complex from prototype foamy virus allowed to investigate the role of the different partners (integrase, DNA, Mg2+ ions, raltegravir) in the complex stability using molecular dynamics (MD) simulations. The presence of Mg2+ ions is found to be essential for the stability, whereas the simultaneous presence of raltegravir and Mg2+ ions has a destabilizing influence. A homology model of HIV‐1 integrase was built on the basis of the X‐ray crystallographic information, and protein marker residues for the ligand binding were detected by clustering the docking poses of known HIV‐1 integrase inhibitors on the model. Interestingly, we had already identified some of these residues to be involved in HIV‐1 resistance mutations and in the stabilization of the catalytic site during the MD simulations. Classification of protein conformations along MD simulations, as well as of ligand docking poses, was performed by using an original learning method, based on self‐organizing maps. This allows us to perform a more in‐depth investigation of the free‐energy basins populated by the complex in MD simulations on the one hand, and a straightforward classification of ligands according to their binding residues on the other hand. Proteins 2014; 82:466–478. © 2013 Wiley Periodicals, Inc. 相似文献
994.
Question: Static sampling designs for collecting spatial data efficiently are being readily utilized by ecologists, however, most ecological systems involve a multivariate spatial process that evolves dynamically over time. Efficient monitoring of such spatio‐temporal systems can be achieved by modeling the dynamic system and reducing the uncertainty associated with the effect of design choice at future observation times. However, can we combine traditional techniques with dynamic methods to find optimal dynamic sampling designs for monitoring the succession of a herbaceous community? Location: Lower Hamburg Bend Conservation Area, Missouri, USA (40°34′42″ lat. 95°45′38″ long.). Methods: The dynamic nature of the system under study is modeled in such a way that uncertainty in the measurements and temporal process can both be accounted for. Both fixed and roving monitoring locations were used in conjunction with a spatio‐temporal statistical model to efficiently determine optimal locations of roving monitors over time based on the reduction of uncertainty in predictions. Results: During the first 3 years of the study, roving monitors where held at fixed locations to allow for statistical parameter estimation from which to make predictions. Optimal monitoring locations for the remaining 2 years were selected based on the overall reduction in prediction uncertainty. Conclusions: The dynamic and adaptive vegetation monitoring scheme allowed for the efficient collection of data that will be utilized for many future ecological studies. By optimally placing an additional set of monitoring locations, we were able to utilize information about the system dynamics when informing the data collection process. 相似文献
995.
Susan E. Gresens Kenneth T. Belt Jamie A. Tang Daniel C. Gwinn Patricia A. Banks 《Hydrobiologia》2007,575(1):173-190
In a longitudinal study of two streams whose lower reaches received unattenuated urban stormwater runoff, physical disturbance
by stormflow was less important than the persistant unidentified chemical impacts of urban stormwater in limiting the distribution
of Chironomidae, and Ephemeroptera, Trichoptera and Plecoptera (EPT). A hierarchical spatial analysis showed that chironomid
density did not decrease from rural to urban stream reaches. Instead, the taxonomic composition of chironomid assemblages
was significantly altered in urban versus rural reaches; chironomid assemblages in urban reaches exhibited higher average
pollution tolerance scores. In contrast, the density of EPT was significantly lower in urban reaches. Despite higher values
of stormflow tractive force in urban reaches, streambed stability tended to be greater in urban reaches. Modeling of temporal
variation in chironomid density showed similar patterns in both rural and urban reaches: chironomid density had a unimodal
relationship to rainfall index (RI), with highest densities at intermediate values of RI. Models of EPT density over time
in rural reaches showed no significant relation to RI, and temporal variation in EPT density in urban reaches was not predictable.
The abundance of fine particulate organic matter, including periphyton (FPOM), on cobbles was greater in urban reaches and
showed a much greater degree of temporal variation than in rural reaches. In urban reaches, a negative relation between FPOM
and RI indicated the importance of stormflow abrasion.
Handling editor: K. Martens 相似文献
996.
Monitoring of three-dimensional floodplain vegetation structure is essential for ecological studies, as well as for hydrodynamic
modelling of rivers. Height and density of submerged vegetation and density of emergent vegetation are the key characteristics
from which roughness parameters in hydraulic models are derived. Airborne laser scanning is a technique with broad applications
in vegetation structure mapping, which therefore may be a promising tool in monitoring floodplain vegetation for river management
applications. This paper first provides an introduction to the laser scanning technique, and reviews previous studies on the
extraction of vegetation height and density of forests, low vegetation and meadows or unvegetated areas. Reliable predictions
using laser scan data have been reported for forest height (R2=0.64–0.98), parameters related to forest density, such as stem number, stem diameter, biomass, timber volume or basal area
(R2=0.42–0.93), and herbaceous vegetation height (summer condition; R2=0.75–0.89). No empirical relations have been reported on density of herbaceous vegetation. Laser data of meadows and unvegetated
areas show too much noise to predict vegetation structure correctly. In a case study for the lower Rhine river, the potential
of laser scan mapping of vegetation structure was further explored for winter conditions. Three laser-derived metrics that
are often reported in the literature have been applied to characterize local vertical distributions of laser reflections.
The laser data clearly show the large structural differences both between and within vegetation units that currently are the
basis of floodplain vegetation and roughness mapping. The results indicate that airborne laser scanning is a promising technique
for extraction of 3D-structure of floodplain vegetation in winter, except for meadows and unvegetated areas. 相似文献
997.
Forest density expressing the stocking status constitutes the major stand physiognomic parameter of Indian forest. Density
and age are often taken as surrogate to structural and compositional changes that occur with the forest succession. Satellite
remote sensing spectral response is reported to provide information on structure and composition of forest stands. The various
vegetation indices are also correlated with forest canopy closure. The paper presents a three way crown density model utilizing
the vegetation indices viz., advanced vegetation index, bare soil index and canopy shadow index for classification of forest
crown density. The crop and water classes which could not be delineated by the model were finally masked from normalized difference
vegetation index and TM band 7 respectively. The rule based approach has been implemented for land use and forest density
classification. The broad land cover classification accuracy has been found to be 91.5%. In the higher forest density classes
the classification accuracy ranged between 93 and 95%, whereas in the lower density classes it was found to be between 82
and 85%. 相似文献
998.
阿布来提·阿布都热西提 《植物研究》2002,22(1):68-71
根据历史资料记载进一步证实新疆是历史悠久的“梨乡” ,而阔他阿木特则为土户梨之一个品种。通过对阔他阿木特形态及结构的分析研究并经过深入的植物检索确定了阔他阿木特在西洋梨属 (Pyruscommunis.L)的一个地方品种地位。通过化学定性定量分析阔他阿木特中不确定之营养成分得以揭示 ,其具有较高的营养成分 相似文献
999.
The detection of vegetational change by multitemporal analysis of LANDSAT data: the effects of goose foraging 总被引:2,自引:1,他引:2
1 The North American mid-continent population of lesser snow geese now exceeds 3 million birds and the population is increasing in the order of 7% per annum. The foraging activities of the birds on Arctic breeding grounds are leading to loss of vegetation and habitat destruction, particularly in coastal areas bordering the Hudson and James Bays.
2 Multitemporal analysis of LANDSAT data has been carried out to detect vegetational change from 1973 to 1993 at La Pérouse Bay and its vicinity, the site of a breeding colony of snow geese.
3 Difference vegetation images (DVI) (difference between infra-red and red images) were prepared from images obtained in late summer in 1973, 1984 and 1993, in order to enhance vegetation density. Pair-wise differences were calculated between these DVI images, which resulted in three, secondary, classified images. Classification of the three secondary images (1973–84, 1984–93, 1973–93) yielded three well-defined classes: water, vegetation decline and no change in vegetation.
4 Histogram counts gave the following values for areas of vegetation decline: 1973–84, 1026 ha; 1984–93, 1428 ha; 1973–93, 2454 ha.
5 The loss of vegetation and the destruction of habitat are discussed in relation to the foraging activities of the expanding goose population. 相似文献
2 Multitemporal analysis of LANDSAT data has been carried out to detect vegetational change from 1973 to 1993 at La Pérouse Bay and its vicinity, the site of a breeding colony of snow geese.
3 Difference vegetation images (DVI) (difference between infra-red and red images) were prepared from images obtained in late summer in 1973, 1984 and 1993, in order to enhance vegetation density. Pair-wise differences were calculated between these DVI images, which resulted in three, secondary, classified images. Classification of the three secondary images (1973–84, 1984–93, 1973–93) yielded three well-defined classes: water, vegetation decline and no change in vegetation.
4 Histogram counts gave the following values for areas of vegetation decline: 1973–84, 1026 ha; 1984–93, 1428 ha; 1973–93, 2454 ha.
5 The loss of vegetation and the destruction of habitat are discussed in relation to the foraging activities of the expanding goose population. 相似文献
1000.