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Neporo4naja [7]
3 years ago
10

What are important facts about weathering

Geography
1 answer:
Tema [17]3 years ago
6 0
<span><em>Weathering is the gradual breakdown of rocks when they are exposed to the air. Weathering affects surface rocks the most, but water trickling into the ground can weather rocks 200 m down. The more extreme the climate, the faster weathering takes place, whether the climate is very cold or very hot. In tropical Africa the basal weathering front (the lowest limit of weathering underground) is often 60 m down. Weathering works chemically (through chemicals in rainwater), mechanically (through temperature changes) and organically (through plants and animals). Chemical weathering is when gases dissolve in rain o form weak acids that corrode rocks such as limestone. Weathering is the breaking up of rocks by agents such as water, ice, chemicals and changing temperature. The main form of mechanical weathering is frost shattering — when water expands as it freezes in cracks in the rocks and so shatters the rock. Thermoclastis is when desert rocks crack as they get hot and expand in the day, then cool and contract at night. Exfoliation is when rocks crack in layers as a weight of rock or ice above them is removed. At 22°C, ice can exert a pressure of 3000 kg on an area of rock the size of a postage stamp. The desert heat means that both the chemical and t he mechanical weathering of the rocks is intense.                                                                                                                                                                                                               Hope this helped
                    </em>
</span>
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The new method, developed in Richard Carson’s lab at Yale’s School of Engineering and Applied Sciences, is based on positron emission tomography (PET), which detects the radiation emitted by radioactive ‘tracers’ that bind to specific proteins or other molecules after being injected into the body. Until now, the density of synapses in the human brain could only be determined by autopsy, using antibodies that bind to and stain specific synaptic proteins, or electron microscopy to examine the fine structure of the tissue.

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They then dissected the brain and took tissue samples from 12 different regions. Closer examination of these samples using antibody staining further revealed that SV2A levels correspond very closely to those of another protein called synaptophysin, which is considered to be the gold standard of synaptic density, and is used widely to estimate synapse numbers in brain tissue samples. Furthermore, SV2A distribution in the tissue samples was very closely correlated to the measurements obtained earlier by the PET scan, demonstrating that SV2A can be used to accurately measure the density of synapses.

Next, the researchers injected their tracer into five healthy human volunteers, and then scanned their brains, to obtain the very first images of synaptic density in the living human brain. The results were comparable to those seen in the monkey, with the radioactive signal peaking in the grey matter of the cortex within 6 to 15 minutes after injection, and then starting to decline steadily shortly afterwards.

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