Carbon dioxide is split to form oxygen gas and carbon compounds _____.

The balanced equation between sodium metal and water to form aqueous sodium hydroxide and hydrogen gas is: 2Na(s) + 2H2O(l) ↔ 2NaOH(aq) + H2 (g)

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Answer:

123 g

Explanation:

1 mole of H₂SO₄ contains 6.02 × 10²³ molecules of H₂SO₄ (Avogadro's number). The moles of H₂SO₄ represented by 7.50 × 10²³ molecules of H₂SO₄ are:

7.50 × 10²³ molecules × (1 mol/ 6.02 × 10²³ molecules) = 1.25 mol

The molar mass of H₂SO₄ is 98.08 g/mol. The mass of H₂SO₄ represented by 1.25 mol is:

1.25 mol × (98.08 g/mol) = 123 g

The mass of 7.5 x 10²³ molecules of H₂SO₄ is 122.5 g.

One mole of a substance contains 6.02 x 10²³ molecules of the substance.

6.02 x 10²³ molecules --------------- one mole of H₂SO₄

7.5 x 10²³ molecules --------------------- ?

[tex]x = \frac{7.5 \times 10^{23}}{6.02 \times 10^{23}} \\\\x = 1.25 \ moles[/tex]

1 mole ------ 98 g/mol

1.25 moles ----- ?

= 1.25 x 98

= 122.5 g

Thus, the mass of 7.5 x 10²³ molecules of H₂SO₄ is 122.5 g.

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The Earth's groundwater and surface water are replenished through the water cycle, with precipitation and evaporation as key processes. Wetlands significantly contribute to groundwater recharge, yet aquifer depletion often outpaces replenishment. Careful resource management is crucial to maintain a sustainable water supply.

The Earth’s groundwater and surface water are replenished through a variety of natural processes that are part of the water cycle. One of the primary ways this occurs is through precipitation such as rain or snow, which can infiltrate the ground to replenish aquifers or run off into rivers and lakes. Groundwater can also be recharged by seepage from surface waters like lakes and rivers, irrigation practices, and the deliberate pumping of water into the ground. Wetlands play a crucial role as recharge areas by allowing surface water to infiltrate the ground rather than running off or evaporating. However, the rate at which aquifers are being depleted often exceeds their replenishment, raising concerns about sustainability and the need for careful water resource management.

Another important process in the water cycle is evaporation, where water changes from a liquid to a gas, becoming water vapor that enters the atmosphere. Energy from the Sun drives this process, evaporating water from various sources including oceans, lakes, and streams. The water vapor will later undergo condensation, form clouds, and return to the surface as precipitation, thus continuing the cycle. It is essential to understand these processes and manage water use to ensure a sustainable supply of fresh water for future generations.

Final answer:

Groundwater is replenished by the infiltration of rain and snowmelt, which percolates down to replenish aquifers. Surface water is replenished directly by precipitation and the discharge from groundwater. However, the depletion of these sources due to overuse is a growing concern for sustainable water availability.

Explanation:

The Earth's groundwater is replenished through a process where rain or snowmelt infiltrates the soil and percolates down to refill aquifers. This process, known as recharge, typically occurs in areas where the ground permits water to soak in, like wetlands, which are effective recharge areas. As groundwater flows, it can also be replenished by seepage from surface waters like lakes and rivers. Surface water, on the other hand, is primarily restored directly from precipitation and also from groundwater when it discharges into rivers and lakes. Additional methods for replenishing groundwater include deliberate pumping of water underground, irrigation practices, and septic systems. However, the rate at which groundwater is being used for drinking and agriculture often exceeds its replenishment rate, leading to concerns about sustainability.

Part of the broader water cycle, groundwater also contributes to the replenishment of surface water. The water cycle describes the journey of water as it evaporates into the atmosphere, condenses into clouds, and falls back to Earth as precipitation. This precipitation either recharges groundwater or flows into surface water bodies, completing the cycle. Despite being a crucial source of fresh water, particularly in arid regions, groundwater reserves are being depleted by overuse in many parts of the world, posing a challenge for future water availability.

The chlorination of ethane produces a mixture of two isomeric dichlorides, cis-1,2-dichloroethene and trans-1,2-dichloroethene.

The chlorination of ethane yields a mixture of two isomeric dichlorides in addition to ethyl chloride. These two isomers are cis-1,2-dichloroethene and trans-1,2-dichloroethene. In cis-1,2-dichloroethene, the two chlorine atoms are on the same side of the molecule, while in trans-1,2-dichloroethene, the two chlorine atoms are on opposite sides of the molecule.

Polarity is crucial because it affects a molecule's solubility, boiling and melting points, and intermolecular interactions. Polar molecules dissolve well in polar solvents, have higher boiling and melting points due to strong dipole-dipole interactions, and can form hydrogen bonds, influencing their behavior and properties in various environments.

1. Solubility: Polar molecules tend to dissolve well in polar solvents (like water) because of the attraction between the partial charges on the molecules and the solvent. Non-polar molecules dissolve better in non-polar solvents (like oils).

2. Boiling and Melting Points: Polar molecules generally have higher boiling and melting points compared to non-polar molecules of similar size because the dipole-dipole interactions (forces between the positive end of one polar molecule and the negative end of another) are stronger than the van der Waals forces present in non-polar molecules.

3. Intermolecular Interactions: Polarity determines the type of intermolecular forces a molecule can participate in, such as hydrogen bonding (a strong type of dipole-dipole interaction found in molecules with N-H, O-H, or F-H bonds), which significantly affects the physical properties and reactivity of the molecule.