1. (i) Concave mirror; f = 35 - 15 = 20 cm (ii) Sharp Image of Distant Tree at 35 cm Mark: The fact that Sunita gets a sharp, well-defined inverted image of a distant tree at the 35 cm mark indicates that the image is formed at the focus of the concave mirror. Because the incident rays parallel to eachRead more

    (i) Concave mirror; f = 35 – 15 = 20 cm
    (ii) Sharp Image of Distant Tree at 35 cm Mark:
    The fact that Sunita gets a sharp, well-defined inverted image of a distant tree at the 35 cm mark indicates that the image is formed at the focus of the concave mirror. Because the incident rays parallel to each other after reflection from concave mirror meets at focus and produce sharp image at focus. This is because, for a concave mirror, when the object is at infinity (distant object), the image is formed at the focal point.
    In this case, the white screen is adjusted until the image of the distant tree is formed at the 35 cm mark, suggesting that the screen is placed at the focal point of the concave mirror.

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  2. When conducting an experiment to demonstrate the release of carbon dioxide (CO2) during respiration, there are several precautions that a student should take to ensure accurate and reliable observations. Here are two important precautions: Ensure Proper Sealing of the Container: Precaution: The contRead more

    When conducting an experiment to demonstrate the release of carbon dioxide (CO2) during respiration, there are several precautions that a student should take to ensure accurate and reliable observations. Here are two important precautions:

    Ensure Proper Sealing of the Container:

    Precaution: The container used to collect the exhaled air must be tightly sealed.
    Reason: Any leakage in the container can lead to the escape of carbon dioxide and compromise the accuracy of the results. To ensure that the observed gas is indeed the exhaled carbon dioxide from respiration, the container must be airtight to prevent the entry of atmospheric air.

    Use an Appropriate Absorbent:

    Precaution: Choose a suitable absorbent to capture the carbon dioxide.
    Reason: To accurately measure the amount of carbon dioxide released during respiration, it’s important to use an appropriate absorbent that selectively captures CO2 without interfering with other gases present in the exhaled air. Commonly used absorbents include soda lime or potassium hydroxide (KOH). Choosing the right absorbent minimizes the risk of absorbing other gases and ensures that the observed changes are primarily due to the release of carbon dioxide.
    These precautions help maintain the integrity of the experimental setup and ensure that the observed changes are attributable to the release of carbon dioxide during respiration, providing reliable and accurate results.
    Hope you like….👍

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  3. A) Benefits of Ozone: i) Stratospheric Ozone Layer: Ozone is crucial in the stratosphere, where it forms the ozone layer. This layer absorbs most of the sun's harmful ultraviolet (UV) radiation, particularly the high-energy UV-B and UV-C rays. By absorbing and blocking these rays, ozone protects lifRead more

    A) Benefits of Ozone:

    i) Stratospheric Ozone Layer: Ozone is crucial in the stratosphere, where it forms the ozone layer. This layer absorbs most of the sun’s harmful ultraviolet (UV) radiation, particularly the high-energy UV-B and UV-C rays. By absorbing and blocking these rays, ozone protects life on Earth from the harmful effects of excessive UV radiation.
    ii) Protection from UV Radiation: We get Protection from UV Radiation. Ozone prevents harmful UV radiation from reaching the Earth’s surface. Ultra Violet (UV) radiation can cause skin cancer, cataracts, and other health issues in humans. It also affects the DNA of living organisms and can harm marine ecosystems, including phytoplankton and coral reefs.

    B) Damaging Effects of Ozone:

    a) Ground-Level Ozone: While ozone in the stratosphere is beneficial, ground-level ozone (tropospheric ozone) is a major component of smog and can be harmful to human health. It can cause respiratory problems, aggravate asthma, and contribute to air quality issues in urban areas.
    b) Ozone Depletion: The release of certain man-made chemicals, such as chlorofluorocarbons (CFCs) and halons, has led to the depletion of ozone in the stratosphere. Ozone depletion allows more UV radiation to reach the Earth’s surface, posing risks to human health, ecosystems, and wildlife.

    Preventing Ozone Layer Depletion:

    a) Montreal Protocol: The most significant international effort to address ozone layer depletion is the Montreal Protocol, adopted in 1987. The protocol aims to phase out the production and consumption of ozone-depleting substances (ODS), such as CFCs, halons, and other chemicals.
    b) Substitute Chemicals: Developing and using alternatives to ozone-depleting substances in various industrial processes, refrigeration, and air conditioning systems is crucial. Many substitutes, such as hydrochlorofluorocarbons (HCFCs) and hydrofluorocarbons (HFCs), have been developed to replace ODS.
    c) Ozone-Friendly Technologies: Encouraging the use of ozone-friendly technologies, appliances, and equipment helps reduce the demand for ODS. This includes promoting energy-efficient appliances that use substances with low or zero ozone-depleting potential.
    d) Public Awareness: It refers increasing public awareness about the importance of protecting the ozone layer and the consequences of ozone depletion is essential. Social education and outreach programs can help individuals make environmentally conscious choices and support policies that safeguard the ozone layer.
    e) Global Co-operation: Ozone depletion is a global issue, and we concern about this. However, international cooperation is crucial. Continued collaboration among nations, industries, and environmental organizations is necessary to monitor ozone levels, enforce regulations, and address emerging challenges.

    By implementing and strengthening these measures, the international community can work together to prevent further depletion of the ozone layer and protect the Earth from the harmful effects of increased UV radiation.

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  4. Based on the provided information, it seems like Riya is conducting experiments to study the length of the foam formed under two different conditions. Observations: Set I: Riya takes 10 ml of distilled water in test tube "A." Adds 5-6 drops of liquid soap. Shakes the test tube. Observation: Foam isRead more

    Based on the provided information, it seems like Riya is conducting experiments to study the length of the foam formed under two different conditions.
    Observations: Set I:
    Riya takes 10 ml of distilled water in test tube “A.”
    Adds 5-6 drops of liquid soap.
    Shakes the test tube.
    Observation: Foam is formed.
    Reason: The addition of liquid soap to water creates a lather or foam due to the formation of soap molecules surrounding air pockets, stabilizing them and creating bubbles.

    And, Set: II will form less foam because it consist of hard water due to the presence of CaSO4.

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