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slamgirl [31]
3 years ago
10

In Philip’s French class, the students are learning how to pronounce closed vowels and open vowels. The students are most likely

studying French __________. A. syntax B. phonemes C. semantics D. morphemes
Chemistry
2 answers:
Sladkaya [172]3 years ago
7 0

Answer:

It sounds like they are studying French phonemes

Explanations:

I just learned this.

DanielleElmas [232]3 years ago
5 0

Answer:

B. Phonemes

I got it right

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PLEASEEEE HELP ASAP!!!!!!!
ankoles [38]

Answer:

15

Explanation:

3 0
4 years ago
2KCIO3 -> 2KCI + 302
grin007 [14]
I uhhh would answer but this is actually confusing
4 0
3 years ago
3. The activation energy of an uncatalyzed reaction is 95 kJ/mol. The addition of a catalyst lowers the activation energy to 55
Margaret [11]

Answer: 1.019\times { 10 }^{ 7 }

Explanation:

4 0
4 years ago
In a coffee cup calorimeter, 1.60 g of NH4NO3 is mixed with 75.0 g of water at an initial temperature of 25.00 degrees C. After
igomit [66]

Answer:

+26.6kJ/mol

Explanation:

The enthalpy of dissolution of NH₄NO₃ is:

NH₄NO₃(aq) + ΔH  → NH₄⁺ + NO₃⁻

Where ΔH is the heat of reaction that is absorbed per mole of NH₄NO₃,

The moles that reacts in 1.60g are (Molar mass NH₄NO₃:80g/mol):

1.60g * * (1mol / 80g) = 0.02 moles reacts

To find the heat released in the coffee cup calorimeter, we must use the equation:

Q = m×ΔT×C

Where Q is heat released,

m is mass of the solution

ΔT is change in temperature (Final temperature - Initial temperature)

C is specific heat of the solution (4.18J/g°C)

Mass of the solution is:

1.60g + 75g = 76.60g

Change in temperature is:

25.00°C - 23.34°C = 1.66°C

Replacing:

Q = m×ΔT×C

Q = 76.60g×1.66°C×4.18J/g°C

Q = 531.5J

This is the heat released per 0.02mol. The heat released per mole (Enthalpy change for the dissolution of NH₄NO₃) is:

531.5J / 0.02mol = 26576J/ mol =

+26.6kJ/mol

<em>+ because the heat is absorbed, the reaction is endothermic-</em>

7 0
3 years ago
What is causing weathering and erosion of rock?
postnew [5]

Answer:

<u>Physical Weathering</u>

Physical or mechanical weathering is the disintegration of rock into smaller pieces. Physical weathering is often caused by atmospheric changes such as heat or freezing temperatures. Frost wedging results when water freezes and expands in crevices, causing the rock to crack. Also, extreme temperature changes such as rapid heating and cooling can cause the rock to expand and contract. Plants cause weathering when roots growing on or under rocks gradually break the rock apart. In addition, animals such as rodents, earthworms, and insects often disrupt and break rock apart by burrowing and digging. The Wind is another force that causes abrasive weathering by blowing sand against rock faces.

<u>Chemical Weathering</u>

Chemical weathering is the disintegration of rock caused by chemical alteration of the mineral structure. According to Tulane University, the main cause of chemical weathering is the presence of weak acids in water coming in contact with the rock. For example, the reaction of carbon dioxide gas in rainwater can produce carbonic acid that dissolves some minerals, especially limestone. Acid rain caused by pollution such as factory and car exhaust is another agent of chemical weathering. Chemical weathering also occurs when iron in rock oxidizes or rusts. In addition, certain types of lichens and fungi growing on rock secrete acids that etch stone surfaces.

<u>Water Erosion</u>

Heavy rainfall and flooding can wash soil, rock, and sediment away into rivers and streams. Water erosion reshapes shorelines and deposits soil in new locations. Materials can be swept away by the water’s force or dissolved in the water and washed away. In addition, when organic material, which helps retain soil structure, is washed from topsoil, the soil becomes more prone to erosion.

<u>Wind Erosion</u>

The Wind is a powerful erosive force, especially when soil is depleted and dry. Sand and soil are swept up and carried away in clouds of dust. A classic example of soil erosion caused by wind and other factors occurred during the “Dust Bowl Years” of the 1930s. Severe drought and wind, combined with 100 years of poor soil management, led to the devastating erosion of topsoil and formation of giant dust clouds that moved across the prairies of the American Great Plains.

<u>Gravity</u>

Gravity is another force that contributes to erosion, especially when combined with slope. Gravity pulls rocks and boulders down mountainsides and chunks of ice down glaciers. Gravitational pull also helps move water laden with dirt and weathered materials to low-lying areas.

Explanation:

All of these cause weathering and erosion.

7 0
3 years ago
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