Microorganisms - Friend and Foe
Leave a slice of bread in a moist corner during the rainy season and within a couple of days grey-white fuzzy patches appear on it. Look closely with a magnifying glass and you will see tiny black rounded dots studding the fuzz. Something living got there, grew, and is now visibly changing the bread — yet nobody put it there and nobody saw it arrive. That something belongs to a vast world of microorganisms, living things so small that most need a microscope to be seen at all, and this chapter is the map of that world. Microorganisms are not one kind of thing. They come in four major groups — bacteria, fungi, protozoa and some algae — plus viruses, a stranger category that can multiply only inside another living cell. They live absolutely everywhere: in a drop of pond water, in garden soil, in ice-cold glaciers and scalding hot springs, and inside your own gut and lungs. What makes this chapter genuinely interesting is that the very same group of organisms that spoils your bread also sets your curd, raises your dosa batter, cures your infections, protects you through vaccination, fertilises the soil under a bean plant, and quietly recycles every dead leaf back into the earth. The same group also causes cholera, malaria, tuberculosis and food poisoning, and can destroy an entire season's wheat crop. This chapter builds the case, section by section, for why microorganisms deserve the title "friend and foe" rather than simply "germs." You will meet Lactobacillus turning milk into curd, yeast raising bread through fermentation, Alexander Fleming's accidental discovery of penicillin, Edward Jenner's invention of vaccination, the housefly and the female Anopheles mosquito as disease carriers, the salting and pickling methods that preserve food, and the nitrogen cycle — the continuous exchange of nitrogen between air, soil, plants and animals that keeps the atmosphere's composition steady. By the end you should be able to say, for any microorganism in the chapter, whether it helps us, harms us, or both — and explain exactly how.
- Microorganisms are living things too small to see unaided; some, like bread mould, are visible with a magnifying glass, but most need a microscope.
- Four major groups — bacteria, fungi, protozoa and some algae — plus viruses, which multiply only inside a host cell.
- They live everywhere: ice-cold climates, hot springs, deserts, marshy land, and inside plant and animal bodies.
- Friendly roles: curd, bread, cake, alcohol and vinegar through fermentation; antibiotics and vaccines; decomposing waste to clean the environment; fixing nitrogen to enrich soil.
- Harmful roles: disease in humans, animals and plants (disease-causing microbes are pathogens), spoiling food, and food poisoning.
- Diseases spreading person-to-person via air, water, food or contact are communicable diseases; carriers like the housefly and female Anopheles or Aedes mosquito spread them.
- Food preservation — salting, sugaring, oil and vinegar, boiling, refrigeration, pasteurisation — all work by stopping microbial growth.
- Rhizobium in leguminous root nodules fixes atmospheric nitrogen; free-living bacteria and algae do the same, and the nitrogen cycle keeps atmospheric nitrogen near a constant 78%.
- Key idea: microorganisms are a vast group of bacteria, fungi, protozoa, algae and viruses that can equally be humanity's greatest allies through fermentation, medicine and soil fertility, or its most persistent foes through disease and food spoilage, and the nitrogen cycle shows how their fixing and releasing of nitrogen keeps the atmosphere in balance.
Microorganisms — bacteria, fungi, protozoa, algae and viruses — are invisible to the naked eye yet shape human life on both sides: as friends through fermentation, antibiotics, vaccines, decomposition and nitrogen fixation, and as foes through pathogens, food spoilage and crop disease, with food preservation and the nitrogen cycle showing how their activity can be managed and put to use.
What this chapter covers
This companion follows the NCERT chapter's own path: what a microorganism is and how the four major groups plus viruses are classified; where they live; the chapter's central theme of microorganisms as friends (curd, bread, alcohol, medicines, soil fertility, cleaning the environment) and as foes (disease in humans, animals and plants, plus food poisoning); and two practical, testable closing sections — food preservation, and the nitrogen cycle. Two derivations unpack the fermentation reaction and the nitrogen cycle pathway step by step; the worked examples reuse the chapter's own activities (the sugar-and-yeast smell test, the 78% nitrogen figure) as solved problems.
The core ideas
What is a microorganism, and how are they grouped
A microorganism (or microbe) is a living organism too small to be seen with the unaided eye. Some, such as the fungus growing on spoiled bread, are just visible with a magnifying glass; most need a microscope — a drop of pond water or settled soil-water examined under one is teeming with tiny moving organisms, exactly what NCERT's Activities 2.1 and 2.2 ask you to observe. Microorganisms fall into four major groups: bacteria (simple single-celled organisms — some harmful like typhoid- and TB-causing types, some allies like Lactobacillus and Rhizobium), fungi (moulds such as bread mould, Penicillium and Aspergillus), protozoa (single-celled organisms such as Amoeba, Paramecium and the malaria parasite Plasmodium) and some algae (microscopic pond forms such as Chlamydomonas and Spirogyra). Viruses are also microscopic but stand apart: a virus multiplies only inside the living cells of a host — a bacterium, plant or animal — and is essentially inert outside one. Cold, influenza and most coughs are viral, and so are more serious diseases like polio and chicken pox. Microorganisms may be single-celled or multicellular, and live in every environment — ice-cold climates, hot springs, deserts, marshy lands, and inside plant and animal bodies including humans — either attached to a host or entirely free-living.
Friendly microorganisms: food, medicine and the environment
Microorganisms make curd, bread, cake and, since ancient times, alcohol. The bacterium Lactobacillus multiplies rapidly in warm milk and converts it into curd — why a spoonful of yesterday's curd stirred into fresh warm milk works as a starter culture. The same bacteria help make cheese and pickles, curd is a key ingredient of rava idli and bhatura batter, and bacteria with yeast ferment idli and dosa batter into light, bubbly batter. Yeast, a single-celled fungus, is central to baking. Added to sugared dough (Activity 2.3), it respires rapidly, converting sugar into carbon dioxide whose trapped bubbles raise the dough — the same gas-trapping that gives baked bread, pastries and cakes their light texture. When yeast instead converts sugar into alcohol in solution, the process is fermentation, discovered by Louis Pasteur in 1857 and used commercially to produce alcohol, wine and vinegar from grain or fruit sugars. Microorganisms also give us medicines and clean the environment. Antibiotics — penicillin, streptomycin, tetracycline, erythromycin — are grown from specific fungi or bacteria and kill or stop disease-causing microbes. Alexander Fleming discovered penicillin by accident in 1929, noticing that a stray mould, Penicillium, killed the bacteria around it on his culture plate. Vaccines work differently: dead or weakened microbes introduced into a healthy body trigger antibodies the body "remembers," giving lasting protection. Edward Jenner discovered the smallpox vaccine in 1798; vaccination has since eradicated smallpox and controls cholera, tuberculosis, polio and hepatitis (the Pulse Polio Programme). Meanwhile bacteria decompose organic waste into harmless, usable substances — a compost pit turns plant waste into manure while plastic in the same pit stays unchanged (Activity 2.5) — and soil bacteria and blue-green algae fix nitrogen from the atmosphere as biological nitrogen fixers, detailed below.
Harmful microorganisms: disease and food poisoning
Disease-causing microorganisms are called pathogens, entering the body through air, water, food, or contact with an infected person or carrier. Diseases spreading this way are communicable diseases — cholera, common cold, chicken pox and tuberculosis are examples; a cold sneeze spreads virus-laden droplets through the air, which is why covering your nose and mouth and keeping distance from an infected person reduces transmission. Some insects and animals act as carriers. The housefly is a mechanical carrier: it picks up pathogens from garbage and excreta and transfers them to uncovered food, so food should stay covered. The female Anopheles mosquito is a biological carrier of the malaria parasite (Plasmodium), and the female Aedes mosquito carries dengue virus; since mosquitoes breed in standing water, keeping coolers, tyres and flower pots dry directly breaks transmission.
| Human disease | Causative microorganism | Mode of transmission | General prevention |
|---|---|---|---|
| Tuberculosis | Bacteria | Air | Isolation of patient; vaccination at suitable age |
| Measles | Virus | Air | Vaccination |
| Chicken pox | Virus | Air or contact | Isolation; keep belongings separate |
| Polio | Virus | Air or water | Vaccination (Pulse Polio Programme) |
| Cholera | Bacteria | Water or food | Boiled drinking water; hygiene; vaccination |
| Typhoid | Bacteria | Water | Boiled drinking water; hygiene |
| Hepatitis A | Virus | Water | Boiled drinking water; vaccination |
| Malaria | Protozoa | Mosquito bite | Mosquito nets, repellents, no standing water |
Microorganisms also cause disease in animals and plants. Anthrax (bacterium Bacillus anthracis, discovered by Robert Koch in 1876) threatens humans and cattle; foot-and-mouth disease of cattle is viral. In plants, citrus canker (bacterial), rust of wheat (fungal) and yellow vein mosaic of bhindi/okra (viral, insect-spread) reduce crop yield and are controlled with chemicals that kill the responsible microbes. Microorganisms growing on stored or cooked food can also produce toxic substances, causing food poisoning — serious illness and, in severe cases, death.
Food preservation: stopping microbial attack
Spoiled food develops a bad smell, taste and colour because microorganisms are growing on it. Food preservation methods all share one principle: stop microorganisms from growing. The chemical method uses salt, edible oils and preservatives such as sodium benzoate and sodium metabisulphite (common in jams and squashes). Common salt preserves meat, fish, amla, raw mango and tamarind by drawing out the moisture bacteria need; sugar preserves jams and jellies the same way; oil and vinegar preserve pickles because bacteria cannot survive in that environment. Boiling kills microorganisms directly, while refrigeration only slows their growth. Pasteurisation, devised by Louis Pasteur, heats milk to about 70 degrees Celsius for 15 to 30 seconds and chills it rapidly — killing harmful microbes without the prolonged heat of boiling, which is why pasteurised packet milk keeps for days unboiled. Sealed, air-tight packaging keeps microbes off dry fruits and vegetables entirely.
Nitrogen fixation and the nitrogen cycle
Our atmosphere is about 78% nitrogen gas by volume, essential to every living cell — yet plants and animals cannot use it directly. It must first be fixed into nitrogen compounds. The bacterium Rhizobium does this inside the root nodules of leguminous plants such as beans and peas, in a symbiotic relationship: the plant shelters and feeds the bacterium, which fixes nitrogen the plant can use. Free-living soil bacteria and blue-green algae fix nitrogen the same way without a host, and lightning fixes a small extra amount directly. Since plants and animals constantly draw fixed nitrogen out of the soil, yet atmospheric nitrogen stays roughly constant, something must return nitrogen to the air just as fast as fixation removes it — the nitrogen cycle, traced step by step in the second derivation below.
The goal here is to explain, in one connected chain of reasoning, why the same living process inside a single-celled fungus called yeast produces two apparently different everyday results: bread that rises in the oven, and a sugar solution that smells strongly of alcohol after a few hours. Both trace back to what yeast does biologically when given sugar and warmth, so the reasoning follows the organism's activity rather than jumping straight to the word "fermentation."
Step 1. Identify the ingredients and the organism. In Activity 2.4, sugar is dissolved in warm water and yeast powder is added, then kept covered and warm for four to five hours; in Activity 2.3, sugar and yeast are kneaded into a soft dough. Both share the same essentials: living yeast cells, dissolved sugar as food, warmth and time.
Step 2. Recognise what yeast does with sugar. With little oxygen available, yeast breaks sugar down incompletely for energy, releasing two waste products: carbon dioxide gas and ethyl alcohol. This incomplete breakdown is exactly what fermentation means, the process Louis Pasteur first described in 1857.
Step 3. Trace the sugar-solution case. Over the warm hours of Activity 2.4, yeast multiplies and ferments the dissolved sugar; carbon dioxide escapes as gas while ethanol accumulates in the liquid, so the strong smell detected afterward is alcohol — direct evidence of fermentation.
Step 4. Trace the dough case with the same process. Inside kneaded dough, yeast again ferments the sugar, but now the carbon dioxide cannot escape through the sticky dough; trapped bubbles swell it and make it rise (Activity 2.3). Baked, those bubbles set into the light, airy texture of bread, pastries and cakes.
Step 5. State the unifying result. One process — yeast fermenting sugar into carbon dioxide and alcohol — explains both outcomes; only the surrounding conditions differ. The same fermentation, scaled up with yeast grown on grain or fruit sugars, is also how alcohol, wine and vinegar are produced commercially.
Go deeper · Derivation B · 1 minThe nitrogen cycle: why atmospheric nitrogen stays near 78 percent
The goal is to explain, as a connected pathway rather than a list of isolated facts, why the nitrogen content of the atmosphere stays roughly constant even though plants, animals and bacteria are constantly moving nitrogen out of the air, through living things, and back again. The reasoning follows one nitrogen atom on a complete round trip.
Step 1. Start with the problem: nitrogen gas is unusable as it is. About 78% of the atmosphere is nitrogen gas, essential to every living cell, yet neither plants nor animals can absorb it directly — the two nitrogen atoms in N2 are bonded too strongly for ordinary metabolism to split. The huge atmospheric reserve is, by itself, biologically useless.
Step 2. Fixation converts the gas into a usable form. Rhizobium, living symbiotically in leguminous root nodules, along with free-living soil bacteria, blue-green algae and a small contribution from lightning, break the strong N2 bond and combine nitrogen into dissolved compounds in the soil. This step, nitrogen fixation, is the only gateway from air into the living world.
Step 3. Plants absorb and build, then animals inherit. Plant roots absorb these compounds and build proteins and chlorophyll. Animals cannot fix or absorb nitrogen directly either; they get it at second hand, by eating plants or animals that ate plants, carrying nitrogen up the food chain.
Step 4. Death and decomposition release nitrogen back into the soil. When plants and animals die or produce waste, bacteria and fungi decompose the nitrogenous matter back into simple soil compounds roots can absorb again — why plant waste becomes fertile manure while plastic in the same pit stays unchanged (Activity 2.5).
Step 5. Denitrification closes the loop. Denitrifying bacteria convert part of the soil's nitrogen compounds back into nitrogen gas, released to the atmosphere. Because this return flow runs continuously alongside fixation, uptake and decomposition, nitrogen keeps cycling rather than draining away, and the atmosphere's nitrogen fraction stays close to 78% — a steady state from fixation and denitrification balancing each other.
Worked examples
Board level - the Activity 2.4 fermentation smell test explained
Boojho sets up Activity 2.4 exactly as in the textbook: dissolving two to three teaspoons of sugar in about 500 mL of warm water, adding half a spoon of yeast powder, then keeping it covered in a warm place for four to five hours. Explain what he will observe when he smells the solution afterward, and why.
Step 1. Identify what has been added: dissolved sugar as food and living yeast as the organism, kept warm to encourage growth.
Step 2. Recall what yeast does to sugar under these conditions: it ferments the sugar, releasing carbon dioxide gas and ethyl alcohol.
Step 3. Over four to five warm hours, the growing yeast population ferments enough dissolved sugar for the alcohol produced to be smelled directly.
Answer: Boojho will smell a distinct odour of alcohol, because the yeast has fermented the dissolved sugar into ethyl alcohol and carbon dioxide gas.
Board level - calculating the nitrogen in a room's air
A closed classroom has an air volume of 200 cubic metres. Using the atmospheric composition given in the chapter, calculate the volume of nitrogen gas present in the room, and explain why plants outside cannot use any of this nitrogen directly.
Step 1. The atmosphere is about 78% nitrogen gas by volume. Volume of nitrogen gas = 78% of 200 cubic metres = 0.78 times 200 = 156 cubic metres.
Step 2. Despite this large volume, plants cannot absorb nitrogen gas directly; the two nitrogen atoms in N2 are too strongly bonded for a plant's ordinary biology to split.
Step 3. The nitrogen must first be fixed by bacteria such as Rhizobium or free-living soil bacteria and cyanobacteria, converting it into dissolved nitrogen compounds that roots can actually absorb.
Answer: The room contains 156 cubic metres of nitrogen gas, but none of it is usable by plants until soil bacteria fix it into nitrogen compounds.
Higher-order thinking (HOTS / olympiad-style) - crop rotation with a legume
A farmer grows wheat every season and finds his yield drops each year unless he buys nitrogen fertiliser. His neighbour instead rotates the field with a season of moong (a legume) every third year, uses far less fertiliser, and still gets a healthy wheat yield. Using Rhizobium and the nitrogen cycle, explain why crop rotation with a legume works, and predict what would happen to soil fertility if the neighbour ploughed the moong plant's roots and stalks back into the soil instead of removing them after harvest.
Step 1. Wheat has no root nodules, so it only draws nitrogen compounds out of the soil to build its own proteins; season after season of wheat alone steadily depletes fixed soil nitrogen, exactly why the first farmer's yield falls without added fertiliser.
Step 2. Moong hosts Rhizobium in root nodules, in a symbiotic relationship: the plant shelters and feeds the bacteria, which fix atmospheric nitrogen into compounds around the roots, adding fixed nitrogen to the soil rather than only removing it.
Step 3. Wheat planted after moong grows in freshly enriched soil, so it needs less purchased fertiliser for the same yield — the neighbour's advantage from crop rotation.
Step 4. If the moong's roots and stalks are ploughed back in rather than removed, decomposer bacteria and fungi break this organic matter down, releasing further nitrogen compounds into the soil — enriching it beyond what standing Rhizobium fixation alone provides.
Answer: Crop rotation with moong works because Rhizobium in its root nodules fixes atmospheric nitrogen into the soil, unlike wheat which only depletes it; ploughing the moong's roots and stalks back in would enrich the soil further, since decomposers would release the nitrogen locked in that buried plant matter. Timing note: allow about three minutes. The chain has four short links — wheat depletes, moong's Rhizobium fixes, rotation transfers the benefit, ploughing-in adds decomposition on top — so write one sentence per link. The trap here is saying "legumes add nitrogen to soil" without naming Rhizobium and the nodules; it is the bacteria, not the plant itself, that fix the nitrogen.
Common traps
Students consistently mix up a handful of facts here, and examiners know it. Watch for: treating viruses as just another "fifth type of bacteria" rather than a case that reproduces only inside a host cell; assuming every microorganism is harmful, when most of the ones you rely on daily (curd, bread, cheese, soil fertility) are friends; confusing a carrier like the housefly, which merely transports pathogens on its body, with the female Anopheles mosquito, inside which the malaria parasite actually develops — different kinds of "carrying." Students often say "boiling and pasteurisation are the same," when pasteurisation is a brief, controlled heat treatment (about 70 degrees Celsius for 15 to 30 seconds, then rapid chilling) rather than full boiling. Another slip is crediting legumes themselves with fixing nitrogen, rather than naming Rhizobium, the bacterium in their root nodules, as the actual fixer. Finally, students forget the nitrogen cycle needs a return path: fixation alone would drain the atmosphere, and denitrification (bacteria converting soil compounds back to nitrogen gas) closes the loop and keeps the 78% roughly constant.
You should be able to…
- Name the four major groups of microorganisms and explain why viruses are treated separately.
- Describe three ways microorganisms help humans (food, medicine, environment, soil) with an example organism for each.
- Explain the difference between an antibiotic and a vaccine, and why antibiotics fail against viral illnesses.
- Define pathogen and communicable disease, with two examples and their mode of transmission.
- Distinguish a mechanical carrier (housefly) from a biological carrier (female Anopheles mosquito).
- List four methods of food preservation and how each stops microbial growth.
- Explain pasteurisation and how it differs from simply boiling milk.
- Describe the Rhizobium-legume symbiosis and name one other way nitrogen gets fixed.
- Trace the nitrogen cycle from atmospheric gas through fixation, plant and animal use, decomposition and denitrification.
Ask the tutor: Ask your tutor to walk through one more disease from Table 2.1 or 2.2 that was not covered in the worked examples here and quiz you on its causative organism, transmission and prevention.
Why does adding a spoon of old curd to warm milk make new curd form faster
The spoon of old curd already contains millions of living Lactobacillus bacteria — a head start rather than waiting for them to arrive by chance. Once introduced, Lactobacillus multiplies rapidly in the warm milk, converting milk sugar into lactic acid, which thickens and sours the milk into curd. This is called a starter culture, and it is why curd-making is reliable and fast at home.
If microorganisms are so useful, why does my doctor tell me to wash my hands and cover food
Both things are true at once: the same broad group contains helpful members, like Lactobacillus and yeast, and harmful members, called pathogens, that cause disease. Washing hands and covering food is not about avoiding all microorganisms; it is about keeping disease-causing pathogens spread by unwashed hands, houseflies or contaminated water away from your body and food. You are surrounded by beneficial microbes constantly; hygiene targets only the pathogenic ones.
Why does packaged pasteurised milk stay fresh for days without me boiling it, but fresh unboiled milk spoils quickly
Pasteurisation already heated the milk to about 70 degrees Celsius for 15 to 30 seconds and rapidly chilled it, killing the great majority of harmful microorganisms that would otherwise spoil it — a controlled step performed before the milk reaches you. Fresh, unboiled milk has not had this treatment, so whatever microorganisms were already present, including ones that spoil milk, keep multiplying at room temperature, which is why it turns sour much faster unless boiled first.
Why does the percentage of nitrogen in the air stay the same even though bacteria are constantly fixing it into the soil
Because nitrogen fixation is only half of a continuous two-way cycle, not a one-way drain. Bacteria like Rhizobium and cyanobacteria are constantly pulling nitrogen gas out of the air into soil compounds; plants absorb these, animals eat the plants, and both eventually die and decompose, releasing nitrogenous matter back into the soil. A separate group of denitrifying bacteria then convert part of it back into nitrogen gas, released to the atmosphere. Fixation removes nitrogen from the air while denitrification returns it, and because the two flows roughly balance, the atmosphere's nitrogen content stays close to a steady 78%.