The reaction needed to remove glucose molecule from a polysaccharide is hydrolysis.
Glucose is a type of monosaccharide which is used in the body for energy.
These monosaccharides such as:
can combine together to form a larger molecule of sugar known as polysaccharides in a reaction called condensation reaction.
Examples of polysaccharides are
These polysaccharides can also be broken down to form the various monosaccharides that makes them up.
The hydrolysis of polysaccharides involves the breaking of the glycosidic bonds that hold the monomers of a polysaccharide molecule together.
This leads to the formation of monosaccharides such as glucose.
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The atmosphere transfers heat energy and moisture across the Earth. Incoming solar radiation (insolation) is redistributed from areas in which there is a surplus of heat (the equator) to areas where there is a heat deficit (the North and South Pole). This is achieved through a series of atmospheric cells: the Hadley cell, the Ferrel cell and the Polar cell (Figure 2). These operate in a similar way to, and indeed interact with, the ocean conveyor.
For example, as the oceans at low latitudes are heated, water evaporates and is transported poleward as water vapour. This warm air eventually cools and subsides. Changes in temperature and CO2 concentrations can lead to: changes in the size of atmospheric cells (in particular, the Hadley cell is susceptible to these alterations); warming in the troposphere; and disproportionately strong warming in Arctic regions. The strong interactions between ocean and atmospheric dynamics, and the significant feedback mechanisms between them, mean that climate researchers must consider these Earth components as interlinked systems. The necessity to assess ocean-atmospheric changes at the global scale has implications for the way in which research is conducted. It is only by integrating palaeo evidence of past changes, with present day monitoring, and projected models,
<span><span>Polar Easterlies
</span><span>Prevailing Westerlies (aka Westerlies).
</span><span>
Tropical Easterlies (aka Trade Winds).
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The fossil record essentially keeps track of the abundance and appearance of various fossils during different time periods. As time goes on, the fossils change. Using the fossil record, we can compare and contrast the fossils to develop theories about changing life forms and their connection to time.
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the the second least force as it go it lose more and more force until it falls when it force the ball to drop the minute it hits the floor it has the least force
