1,086 research outputs found

    Uncertainties in selected river water quality data

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    International audienceMonitoring of surface waters is primarily done to detect the status and trends in water quality and to identify whether observed trends arise from natural or anthropogenic causes. Empirical quality of river water quality data is rarely certain and knowledge of their uncertainties is essential to assess the reliability of water quality models and their predictions. The objective of this paper is to assess the uncertainties in selected river water quality data, i.e. suspended sediment, nitrogen fraction, phosphorus fraction, heavy metals and biological compounds. The methodology used to structure the uncertainty is based on the empirical quality of data and the sources of uncertainty in data (van Loon et al., 2005). A literature review was carried out including additional experimental data of the Elbe river. All data of compounds associated with suspended particulate matter have considerable higher sampling uncertainties than soluble concentrations. This is due to high variability within the cross section of a given river. This variability is positively correlated with total suspended particulate matter concentrations. Sampling location has also considerable effect on the representativeness of a water sample. These sampling uncertainties are highly site specific. The estimation of uncertainty in sampling can only be achieved by taking at least a proportion of samples in duplicates. Compared to sampling uncertainties, measurement and analytical uncertainties are much lower. Instrument quality can be stated well suited for field and laboratory situations for all considered constituents. Analytical errors can contribute considerably to the overall uncertainty of river water quality data. Temporal autocorrelation of river water quality data is present but literature on general behaviour of water quality compounds is rare. For meso scale river catchments (500?3000 km2) reasonable yearly dissolved load calculations can be achieved using biweekly sample frequencies. For suspended sediments none of the methods investigated produced very reliable load estimates when weekly concentrations data were used. Uncertainties associated with loads estimates based on infrequent samples will decrease with increasing size of rivers

    Uncertainties in selected surface water quality data

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    International audienceMonitoring of surface waters is primarily done to detect the status and trends in water quality and to identify whether observed trends arise form natural or anthropogenic causes. Empirical quality of surface water quality data is rarely certain and knowledge of their uncertainties is essential to assess the reliability of water quality models and their predictions. The objective of this paper is to assess the uncertainties in selected surface water quality data, i.e. suspended sediment, nitrogen fraction, phosphorus fraction, heavy metals and biological compounds. The methodology used to structure the uncertainty is based on the empirical quality of data and the sources of uncertainty in data (van Loon et al., 2006). A literature review was carried out including additional experimental data of the Elbe river. All data of compounds associated with suspended particulate matter have considerable higher sampling uncertainties than soluble concentrations. This is due to high variability's within the cross section of a given river. This variability is positively correlated with total suspended particulate matter concentrations. Sampling location has also considerable effect on the representativeness of a water sample. These sampling uncertainties are highly site specific. The estimation of uncertainty in sampling can only be achieved by taking at least a proportion of samples in duplicates. Compared to sampling uncertainties measurement and analytical uncertainties are much lower. Instrument quality can be stated well suited for field and laboratory situations for all considered constituents. Analytical errors can contribute considerable to the overall uncertainty of surface water quality data. Temporal autocorrelation of surface water quality data is present but literature on general behaviour of water quality compounds is rare. For meso scale river catchments reasonable yearly dissolved load calculations can be achieved using biweekly sample frequencies. For suspended sediments none of the methods investigated produced very reliable load estimates when weekly concentrations data were used. Uncertainties associated with loads estimates based on infrequent samples will decrease with increasing size of rivers

    The steering gaits of sperm

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    Sperm are highly specialized cells, which have been subject to substantial evolutionary pressure. Whereas some sperm features are highly conserved, others have undergone major modifications. Some of these variations are driven by adaptation to mating behaviours or fitness at the organismic level. Others represent alternative solutions to the same task. Sperm must find the egg for fertilization. During this task, sperm rely on long slender appendages termed flagella that serve as sensory antennas, propellers and steering rudders. The beat of the flagellum is periodic. The resulting travelling wave generates the necessary thrust for propulsion in the fluid. Recent studies reveal that, for steering, different species rely on different fundamental features of the beat wave. Here, we discuss some examples of unity and diversity across sperm from different species with a particular emphasis on the steering mechanisms. This article is part of the Theo Murphy meeting issue β€˜Unity and diversity of cilia in locomotion and transport’

    Ensuring metrological control of the means of thermal control

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    Π’ настоящСС врСмя всС большСС ΠΏΡ€ΠΈΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ Π½Π°Π±ΠΈΡ€Π°ΡŽΡ‚ ΠΏΡ€ΠΈΠ±ΠΎΡ€Ρ‹ бСсконтактного ΠΈ быстродСйствСнного контроля Ρ‚Π΅ΠΌΠΏΠ΅Ρ€Π°Ρ‚ΡƒΡ€Ρ‹ ΠΏΡ€ΠΈΠ±ΠΎΡ€Π°ΠΌΠΈ, Ρ€Π΅Π³ΠΈΡΡ‚Ρ€ΠΈΡ€ΡƒΡŽΡ‰ΠΈΠΌΠΈ излучСния Π² свСтовом ΠΈ инфракрасном Π΄ΠΈΠ°ΠΏΠ°Π·ΠΎΠ½Π°Ρ….At present, more and more devices are being used to collect non-contact and high-speed temperature control instruments that register radiation in the light and infrared ranges

    Diurnal versus spatial variability of greenhouse gas emissions from an anthropogenically modified lowland river in Germany

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    Greenhouse gas (GHG) emissions from rivers are globally relevant, but quantification of these emissions comes with considerable uncertainty. Quantification of ecosystem-scale emissions is challenged by both spatial and short-term temporal variability. We measured spatio-temporal variability of CO2 and CH4 fluxes from a 1 km long reach of the lowland river Elbe in Germany over 3 d to establish which factor is more relevant to be taken into consideration: small-scale spatial variability or short-term temporal variability of CO2 and CH4 fluxes. GHG emissions from the river reach studied were dominated by CO2, and 90 % of total emissions were from the water surface, while 10 % of emissions were from dry fallen sediment at the side of the river. Aquatic CO2 fluxes were similar at different habitats, while aquatic CH4 fluxes were higher at the side of the river. Artificial structures to improve navigability (groynes) created still water areas with elevated CH4 fluxes and lower CO2 fluxes. CO2 fluxes exhibited a clear diurnal pattern, but the exact shape and timing of this pattern differed between habitats. By contrast, CH4 fluxes did not change diurnally. Our data confirm our hypothesis that spatial variability is especially important for CH4, while diurnal variability is more relevant for CO2 emissions from our study reach of the Elbe in summer. Continuous measurements or at least sampling at different times of the day is most likely necessary for reliable quantification of river GHG emissions.</p

    Deep inelastic collisions between very heavy nuclei

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    Π“ΠΎΡ€ΠΈΠ·ΠΎΠ½Ρ‚Π°Π»ΡŒΠ½Ρ‹Π΅ классификаторы. ΠžΡΠ½ΠΎΠ²Ρ‹ Ρ‚Π΅ΠΎΡ€ΠΈΠΈ ΠΈ расчСта: ΠΌΠΎΠ½ΠΎΠ³Ρ€.

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    ΠŸΡ€ΠΈΠ²Π΅Π΄Π΅Π½Ρ‹ тСхнологичСскиС схСмы получСния ΡΡ‚Ρ€ΠΎΠΈΡ‚Π΅Π»ΡŒΠ½Ρ‹Ρ… пСсков ΠΏΡ€ΠΈ Π³ΠΈΠ΄Ρ€ΠΎΠΌΠ΅Ρ…Π°Π½ΠΈΠ·ΠΈΡ€ΠΎΠ²Π°Π½Π½ΠΎΠΉ Π΄ΠΎΠ±Ρ‹Ρ‡Π΅, основныС конструктивныС схСмы классификаторов, ΠΈΡΠΏΠΎΠ»ΡŒΠ·ΡƒΠ΅ΠΌΡ‹Ρ… ΠΏΡ€ΠΈ ΠΏΠΎΠ»ΡƒΡ‡Π΅Π½ΠΈΠΈ ΡΡ‚Ρ€ΠΎΠΈΡ‚Π΅Π»ΡŒΠ½Ρ‹Ρ… пСсков. ОсобоС Π²Π½ΠΈΠΌΠ°Π½ΠΈΠ΅ ΡƒΠ΄Π΅Π»Π΅Π½ΠΎ ΠΈΠ·ΡƒΡ‡Π΅Π½ΠΈΡŽ процСсса взаимодСйствия ΠΏΡ€ΠΎΡ‚ΠΎΡ‡Π½ΠΎΠΉ части Π³ΠΎΡ€ΠΈΠ·ΠΎΠ½Ρ‚Π°Π»ΡŒΠ½ΠΎΠ³ΠΎ классификатора с ΡΠΎΠ²ΠΎΠΊΡƒΠΏΠ½ΠΎΡΡ‚ΡŒΡŽ Ρ‚Π²Π΅Ρ€Π΄Ρ‹Ρ… частиц, располоТСнных Π² Π³ΠΎΡ€ΠΈΠ·ΠΎΠ½Ρ‚Π°Π»ΡŒΠ½ΠΎΠΌ ускорСнном ΠΏΠΎΡ‚ΠΎΠΊΠ΅ нСсущСй срСды. Π’Ρ‹ΠΏΠΎΠ»Π½Π΅Π½ΠΎ матСматичСскоС ΠΌΠΎΠ΄Π΅Π»ΠΈΡ€ΠΎΠ²Π°Π½ΠΈΠ΅ ускорСнного двиТСния Π³ΠΎΡ€ΠΈΠ·ΠΎΠ½Ρ‚Π°Π»ΡŒΠ½ΠΎΠ³ΠΎ ΠΏΠΎΡ‚ΠΎΠΊΠ° ΠΈ Ρ‚Π²Π΅Ρ€Π΄Ρ‹Ρ… частиц Π² ΠΏΡ€Π΅Π΄Π΅Π»Π°Ρ… Ρ€Π°Π·Π½ΠΎΠ½Π°ΠΊΠ»ΠΎΠ½Π½Ρ‹Ρ… повСрхностСй Π³ΠΎΡ€ΠΈΠ·ΠΎΠ½Ρ‚Π°Π»ΡŒΠ½ΠΎΠ³ΠΎ классификатора. Π­ΠΊΡΠΏΠ΅Ρ€ΠΈΠΌΠ΅Π½Ρ‚Π°Π»ΡŒΠ½ΠΎ ΠΈΠ·ΡƒΡ‡Π΅Π½ΠΎ Π³Ρ€Π°Π²ΠΈΡ‚Π°Ρ†ΠΈΠΎΠ½Π½ΠΎΠ΅ осаТдСниС Ρ‚Π²Π΅Ρ€Π΄Ρ‹Ρ… частиц, рассмотрСнноС Π² Π²ΠΈΠ΄Π΅ Π²Π΅Ρ€Ρ‚ΠΈΠΊΠ°Π»ΡŒΠ½ΠΎΠΉ ΠΈ Π³ΠΎΡ€ΠΈΠ·ΠΎΠ½Ρ‚Π°Π»ΡŒΠ½ΠΎΠΉ ΡΠΎΡΡ‚Π°Π²Π»ΡΡŽΡ‰ΠΈΡ…, Π° Ρ‚Π°ΠΊΠΆΠ΅ влияниС стСснСнности двиТСния ΠΈ пСрСмСщСния Ρ‚Π²Π΅Ρ€Π΄Ρ‹Ρ… частиц ΠΎΡ‚Π½ΠΎΡΠΈΡ‚Π΅Π»ΡŒΠ½ΠΎ нСсущСго Π³ΠΎΡ€ΠΈΠ·ΠΎΠ½Ρ‚Π°Π»ΡŒΠ½ΠΎΠ³ΠΎ ΠΏΠΎΡ‚ΠΎΠΊΠ°. ΠŸΡ€ΠΈΠ²Π΅Π΄Π΅Π½Π° ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΈΠΊΠ° расчСта ΠΈ Π²Ρ‹Π±ΠΎΡ€Π° ΠΏΠ°Ρ€Π°ΠΌΠ΅Ρ‚Ρ€ΠΎΠ² классификаторов, информация ΠΎΠ± ΠΎΠΏΡ‹Ρ‚Π΅ проСктирования ΠΈ внСдрСния Π³ΠΎΡ€ΠΈΠ·ΠΎΠ½Ρ‚Π°Π»ΡŒΠ½Ρ‹Ρ… классификаторов Π² составС Π΄ΠΎΠ±Ρ‹Ρ‡Π½Ρ‹Ρ… комплСксов ΠΏΡ€ΠΈ освоСнии ΠΎΠ±Π²ΠΎΠ΄Π½Π΅Π½Π½Ρ‹Ρ… мСстороТдСний пСсков. ΠœΠΎΠ½ΠΎΠ³Ρ€Π°Ρ„ΠΈΡ ΠΌΠΎΠΆΠ΅Ρ‚ Π±Ρ‹Ρ‚ΡŒ ΠΏΠΎΠ»Π΅Π·Π½Π° студСнтам, ΠΈΠ½ΠΆΠ΅Π½Π΅Ρ€Π½ΠΎ-тСхничСским Ρ€Π°Π±ΠΎΡ‚Π½ΠΈΠΊΠ°ΠΌ, сотрудникам Π²Ρ‹ΡΡˆΠΈΡ… ΡƒΡ‡Π΅Π±Π½Ρ‹Ρ… Π·Π°Π²Π΅Π΄Π΅Π½ΠΈΠΉ, Π½Π°ΡƒΡ‡Π½ΠΎ-ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Ρ‚Π΅Π»ΡŒΡΠΊΠΈΡ… институтов ΠΈ ΠΏΡ€ΠΎΠ΅ΠΊΡ‚Π½Ρ‹Ρ… ΠΎΡ€Π³Π°Π½ΠΈΠ·Π°Ρ†ΠΈΠΉ Π³ΠΎΡ€Π½ΠΎΠΉ ΠΏΡ€ΠΎΠΌΡ‹ΡˆΠ»Π΅Π½Π½ΠΎΡΡ‚ΠΈ
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