☰ Year plan · Science

Blood pressure, wind, plant tissues and humidity

Week 12 · 2-3 Physical Factors (B): blood pressure, wind and wind systems, wind speed and plant tissues, humidity, effects of humidity on people and living things, osmoregulation, the data-collection activities · 3 lessons
3

Humidity and the body's water balance

Integrated Science Sec 1 Term 1, Unit 2: pp. 90–97
GoalDefine relative humidity, explain how humidity affects the body, and describe osmoregulation.
New words
humidity · the amount of water vapour in the airrelative humidity · the water vapour in the air as a percentage of the most it can hold at that temperaturehygrometer · an instrument that measures humidityosmoregulation · keeping the water and salts of the body in balance
Explanation

Humidity is the water vapour in the air. Warmer air can hold more vapour. Air is saturated when it holds the most it can at that temperature and pressure. Relative humidity = (vapour present ÷ the most the air could hold at that temperature) × 100%. A hygrometer measures humidity, and 40% to 60% is comfortable. Sweat cools us only as it evaporates, because evaporation takes heat from the skin. In humid air sweat evaporates slowly, so the body cools poorly, we feel hotter and tired, and long exposure risks heat stress or heatstroke; humid heat feels worse because sweat cannot evaporate, not because the air is hotter. In dry air sweat evaporates fast, and skin and the lining of the nose and airways dry out, which risks infection and dehydration. Drink water and ask an adult if you feel unwell. Osmoregulation keeps water and salts in balance, which is needed for normal blood pressure and for cells to work. In dry air the body loses more water through sweat and breath; receptors in the brain sense this and the kidneys reabsorb more water, giving concentrated urine. The kidneys reabsorb water; they do not make it. In humid air plants lose water more slowly by transpiration, so less water and salts are pulled up the stem.

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Worked examples
Find the relative humidity. The air holds 10 g of vapour in each cubic metre, and at this temperature it could hold at most 20 g. RH = 10 ÷ 20 × 100 = 50%.
Why does the same vapour give a higher RH in colder air? Air with 9 g/m³ that could hold 18 g has RH 50%. When it cools to a temperature at which it could hold only 12 g, RH = 9 ÷ 12 × 100 = 75%.
Read the invented day: humidity is highest early at 70% when the air is coolest, and lowest at 15 h with 30%, the hottest part of the day. This is the usual pattern, because warm air can hold more vapour.
Class activity

Wet and dry cloth, with a grown-up. Wet one cloth, keep a second dry, and put each on a different forearm in a gentle breeze. Say which feels cooler and why (evaporation takes heat). Wash your hands after. Then put a damp paper towel in a sealed bag and another in an open space for a day and describe the difference. Finally read the humidity from a weather app on two days and say which day sweat would evaporate faster.

Practice
1
Air holds 6 g of vapour per m³ and could hold at most 24 g. Find the relative humidity.
2
Why does humid heat feel worse than dry heat?
3
What do the kidneys do when the body is short of water?
4
Why does dry air dry out the nose and airways?
5
What range of relative humidity is comfortable?