Potassium ion would most likely bond with chlorine
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The main active components of bleach and many other household cleaners are salts. Salts are produced by mixing of acid and bases along with water. There are three different types of salts such as acidic salt, basic salts, and neutral salts.
The different products of salts are used in daily household detergents. The common salt products are bleaching powder, caustic soda, washing soda. Caustic soda is present in detergents, soaps, chlorine is present in bleaching powder. Washing soda is used in soaps.
The general journal of Smith Auto will be the first place where the company will record its data.
<h3>What is a journal?</h3>
The general journal is illustrated below:
July 3:
Debit inventory $3100
Credit Account payable $3100
July 6:
Debit Cash $600
Credit Sales revenue $600
Debit Cost of goods sold $450
Credit Inventory $450
July 7
Debit Equipment $5000
Credit Capital $5000
July 9
Debit Account receivable $750.
Credit Equipment $750
July 13
Debit Account receivable Bell $3200
Credit Sales revenue $3200
Debit Cost of goods sold = $2800
Credit Inventory = $2800
July 15
Debit Sales return $500
Credit Account receivable $500
July 22
Debit Building $20000
Credit Notes payable $20000
July 26
Debit Salaries expense $4400
Credit Cash $4400
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Answer:
1. Because it is thick and has relatively low density, continental crust rises higher on the mantle than oceanic crust, which sinks into the mantle to form basins. When filled with water, these basins form the planet's oceans.The lithosphere is the outermost mechanical layer, which behaves as a brittle, rigid solid.
3. Earth's inner core is solid because it is under such intense pressure from the weight of the entire planet that its atoms are held together by force. ... ... By contrast, the outer layers of Earth, while being slightly cooler (but still incredibly hot), have less pressure and thus their atomic form reverts to liquid.
4. Scientists have learned about Earth's internal structure by studying how these waves travel through the Earth. The technique is straightforward — it involves measuring the time it takes for both types of waves to reach seismic stations from the epicenter of an earthquake.
