Controls on the chemical composition of Alpine glacial meltwaters.

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  • English
University of East Anglia , Norwich
ID Numbers
Open LibraryOL14509399M

Solute acquisition by Alpine glacial meltwaters is the result of the coupling of different pairs of reactions, one of which usually involves dissolved gases. Hence, the availability of atmospheric gases to solution is an important control on the composition of glacial meltwaters.

A new method of hydrograph separation for bulk meltwaters draining Alpine glaciers is proposed.

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It is based on the two-component (subglacial and englacial) mixing model of Collins (), but allows the composition of the subglacial component to vary between ascending and descending lines of the mean englacial component can be derived from linear relationships between sulphate Cited by:   The temperature of ice exerts an important control on a wide variety of glacial processes (Benn and Evans, ), including those which influence chemical weathering and the composition of meltwaters in glacierised environments (e.g.

meltwater flow, sediment production, gas availability).Cited by:   An assessment was made of the mean levels of major and trace elements and of biogenic and organic matter in glacial and river waters within the Aktru river basin (Gornyi Altai, Russia). The analysis showed a general tendency for an increase in mineralization along the direction from the region of alimentation of glaciers to the mouth of the river.

A relatively abrupt increase was revealed in Cited by: 3. The O 2 content of glacial meltwaters depends on the initial content of snow and icemelt, which may be controlled by the rate of melting, and the kinetic balance between O 2 losses (e.g. sulphide oxidation, microbial respiration) and gains (e.g.

diffusion of O 2 into solution).Cited by: Controls on the major-ion chemistry of the Dokriani glacier meltwaters, Ganga basin, Garhwal Himalaya, India, Journal of Glaciology, Vol (), Meltwaters collected from boreholes drilled to the base of the Haut Glacier d'Arolla, Switzerland have chemical compositions that can be classified into three main groups.

The volume of water moving through the subglacial network is a primary control on the Sr composition of subglacial meltwater. Increases in discharge correspond to lower subglacial residence times, driving the meltwater chemistry away from carbonate saturation and allows for an increase in calcite weathering.

Physical and chemical analyses. Ice samples (after melting) and meltwaters were analyzed for dry mass (DM), pH, total organic carbon, total organic nitrogen, and total organic phosphorus using standard methods (Hunt & Wilson, ).

Sediment samples were analyzed for the same components according to Mudroch et al. Microbiological analyses. Books; Other Publications. ; Eos Archives () Angela Gurnell, A conceptual model of solute acquisition by Alpine glacial meltwaters, Journal of Glaciology, /S Sigurdur R.

Gislason, The chemical composition of rivers and snow affected by the / Bárðarbunga eruption, Iceland, Journal. Alpine glaciers have receded substantially over the last century in many regions of the world. Resulting changes in glacial runoff not only affect the hydrological cycle, but can also alter the physical (i.e., turbidity from glacial flour) and biogeochemical properties of downstream ecosystems.

Here we compare nutrient concentrations, transparency gradients, algal biomass, and fossil diatom. Andrew C. Mitchell, Giles H.

Brown, Diurnal hydrological – physicochemical controls and sampling methods for minor and trace elements in an Alpine glacial hydrological system, Journal of Hydrology, /l, (), ().

We compile data showing that, as hypothesized previously, waters draining glaciers have solute chemistry that is distinct from nonglacial rivers and reflects different proportions of mineral weathering reactions.

Elevated pyrite oxidation during glacial weathering could generate acidity, releasing carbon to the atmosphere. We show that this effect could contribute to changes in CO2. The discharge of meltwaters from glaciers or ice sheets into a lake or coastal area can affect planktonic organisms by several other mechanisms that do not involve a direct effect of glacial flour.

For example, the massive discharge of glacier meltwaters into coastal fjords has been implicated in extensive zooplankton mortality (Weslawski and. The recent and rapid recession of alpine glaciers over the last years has major implications for associated aquatic communities.

Glacial meltwater shapes many of the physical features of high altitude lakes and streams, producing turbid environments with distinctive hydrology patterns relative to.

(ii) Controls of δ 30 Si DSi composition of glacial meltwaters.

Details Controls on the chemical composition of Alpine glacial meltwaters. EPUB

Statistical analyses of these data, such as regression model and principal component analysis, do not reveal any significant relationships to suggest an overriding process that is the main cause of the light Si isotopic composition in glacial meltwaters.

Solute yields, laboratory dissolution data and both chemical and isotopic markers of rock weathering reactions are used to characterise the biogeochemistry of glacial meltwaters draining a maritime Antarctic glacier. We find that delayed flowpaths through ice-marginal talus and moraine sediments are critical for the acquisition of solute from rock minerals because delayed flowpaths.

Casassa G, López P, Pouyaud B, Escobar F. Detection of changes in glacial run-off in alpine basins: examples from North America, the Alps, central Asia and the Andes.

Hydrol. Process. ; – Chanudet V, Filella M. Size and composition of inorganic colloids in a peri-alpine, glacial flour-rich lake. Geochim. Cosmochim. Acta. ; Features left by valley glaciers and ice sheets.

Moraines left by valley glaciers are shown in Figure 1, and features left by a receding ice sheet are shown in Figure 2. Moraines are deposits of till that are left behind when a glacier recedes or that are carried on top of alpine l moraines consist of rock debris and sediment that have worked loose from the walls beside a valley.

The chemistry of alpine glacial meltwaters has been used to determine water routing through Alpine glaciers. Water routing, in turn, controls glacier shape, velocity and erosive capacity (Collins, ,; Drewry, ).

These early studies paid little attention to the. Tranter M, Brown G, Raiswell R, Sharp M and Gurnell A A conceptual model of solute acquisition by Alpine glacial meltwaters J.

Glaciol. 39 –81 Crossref Tranter M, Sharp M J, Brown G H, Willis I C, Hubbard B P, Nielsen M K, Smart C C, Gordon S, Tulley M and Lamb H R Variability in the chemical composition of in situ subglacial.

Description Controls on the chemical composition of Alpine glacial meltwaters. EPUB

Precautions and controls. Chemical models of solute acquisition in glacial meltwaters. Glaciol. Controls on the chemical composition of Alpine glacial meltwaters. Ph.D. thesis. University of East Anglia, East Anglia, United Kingdom. The formation and movement of sediments in glacial environments is shown diagrammatically in Figure There are many types of glacial sediment generally classified by whether they are transported on, within, or beneath the glacial ice.

The main types of sediment in a glacial. Water plays a dominant role in many glacial processes and the erosional, depositional and climatic significance of meltwaters and associated fluvioglacial processes cannot be overemphasized.

At its maximum extent c. 20, years ago, the volume of the Laurentide ice sheet was 33 × 10 6 km 3 (about the same as the volume of all ice present today on planet Earth). Researchers report that glacial meltwaters in Canada, containing little organic matter and abundant carbonate and silicate mineral sediments, are a net carbon dioxide sink due to the consumption.

An ice age is a long period of reduction in the temperature of the Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine 's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the is currently in the Quaternary glaciation, known in popular terminology as the.

Impact of Post-Mixing Chemical Reactions on the Major Ion Chemistry of Bulk Meltwaters Draining the Haut Glacier d'Arolla, Valais, Switzerland (G. Brown, et al.). Experimental Investigations of the Weathering of Suspended Sediment by Alpine Glacial Meltwater (G.

Brown, et al.). The weight of glacial ice sheets depress the lithosphere into the mantle causing the crust to subside. After the ice melts, the depressed lithosphere rebounds.

The rebound process is still taking place today (see figures in your text). Sea Level Changes. During glacial periods much sea water was tied up in glaciers so sea level was lower.

Lake - Lake - Basins formed by glaciation: The basin-forming mechanism responsible for the most abundant production of lakes, particularly in the Northern Hemisphere, is glaciation.

The Pleistocene glaciers, which seem to have affected every continent, were especially effective in North America, Europe, and Asia. The retreat of ice sheets produced basins through mechanical action and through. Chemical models of solute acquisition in glacial meltwaters, Journal of Glaciology 30(), Rand McNally ().

The Atlas of the Oceans, Rand McNally and Co., Chicago, pp. Seasonal snow cover exerts a fundamental control upon biological production in underlying habitats: a problem that is best understood in the context of soil and tundra ecology in boreal and Arctic landscapes (e.g. Luus et al ).Interestingly, in the context of glacial snowpacks, changes in the distribution and persistence of snow cover are reasonably well known through mass balance .Impact of Post-Mixing Chemical Reactions on the Major Ion Chemistry of Bulk Meltwaters Draining the Haut Glacier d'Arolla, Valais, Switzerland (G.

Brown, et al.). Experimental Investigations of the Weathering of Suspended Sediment by Alpine Glacial Meltwater (G. Brown, et al.).Price: $"The cold glacial meltwaters flowing from the Antarctic cause a slowing of the currents which enable the ocean to draw down carbon dioxide and heat from the atmosphere," Silvano said.