Question map
Consider the following statements : Statement-I : The soil in tropical rain forests is rich in nutrients. Statement-II : The high temperature and moisture of tropical rain forests cause dead organic matter in the soil to decompose quickly. Which one of the following is correct in respect of the above statements?
Explanation
The correct answer is Option 4 because Statement-I is incorrect, while Statement-II is correct.
Contrary to common perception, the soil in tropical rainforests is nutrient-poor (oxisols/ultisols). While these regions support lush vegetation, the heavy and frequent rainfall leads to intense leaching, where essential soluble nutrients are washed away deep into the subsoil, leaving the topsoil acidic and deficient in minerals.
Statement-II accurately explains the underlying biological process. The high temperature and constant moisture create an ideal environment for decomposers (bacteria and fungi). Consequently, dead organic matter (leaf litter) decomposes extremely rapidly. Rather than being stored in the soil as humus, these nutrients are almost immediately reabsorbed by the dense root systems of the standing vegetation to support quick growth. Thus, the nutrients are locked in the biomass rather than the soil itself, making Statement-I false and Statement-II true.
PROVENANCE & STUDY PATTERN
Full viewThis is a classic 'Conceptual Paradox' question found in every standard Geography NCERT. It tests the counter-intuitive fact that the world's lushest forests grow on some of the world's poorest soils. If you relied on 'common sense' (more trees = better soil), you walked into the trap.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Statement 1: Are soils in tropical rain forests rich in nutrients?
- Statement 2: Do high temperature and high moisture in tropical rain forests cause dead organic matter in the soil to decompose quickly?
- Statement 3: Does the rapid decomposition of dead organic matter caused by high temperature and moisture explain why tropical rain forest soils are rich in nutrients?
- Explicitly states tropical soils are heavily leached.
- Says only a small, temporary fertility is added by burning and is lost after 2–3 crops, implying low inherent soil fertility.
- Identifies rainforest soils as red latosols (lateritic soils) typical of tropical regions.
- Specifies the characteristic soil type (red latosols), supporting inference about distinctive tropical soil properties relevant to nutrient status.
- Directly links warm temperatures and abundant moisture to rapid bacterial breakdown of dead plant matter.
- Explains rapid nutrient release and immediate root uptake, producing soils low in organic matter (humus).
- States bacterial growth is intense in humid tropical/equatorial climates, accelerating decomposition.
- Specifies dead vegetation is rapidly oxidized in these climates, leaving very low humus content.
- Notes a year‑round growing season in equatorial regions, so decay occurs continuously rather than seasonally.
- Links high temperature and abundant rainfall to luxuriant forests where continuous turnover (growth + decay) is possible.
- Explicitly identifies temperature and soil moisture as the most important climatic factors regulating decomposition.
- States that a warm and moist environment favours decomposition, linking high temperature/moisture to faster breakdown of organic matter.
- Describes decomposers as organisms that degrade dead organic matter (detritus).
- Says decomposers break down dead and waste materials into simple absorbable substances, connecting decomposition to nutrient release.
- Notes that changes in temperature and moisture affect decomposition rates, indicating a direct climate–decomposition link.
- Provides a nuance that deviations beyond optimal temperature/moisture can reduce decomposition, qualifying the simple high-temperature/high-moisture explanation.
States that warm temperatures and abundant moisture cause dead plant matter to rapidly decompose and that nutrients released by decay are quickly absorbed by roots, leaving the soil low in organic matter (humus).
A student could combine this with the basic fact that tropical zones are warm and wet to infer decomposition is rapid there and then ask whether rapid uptake by plants leaves little nutrient storage in the soil.
Explains a general rule: in humid tropical climates bacterial growth is intense and dead vegetation is rapidly oxidised, so humus accumulates in cold climates but not in warm ones.
Using the rule plus knowledge that tropics are warm/wet, a student could predict low humus and then test whether that implies soils are nutrient-poor or nutrient-rich at different timescales.
Gives a process (leaching by torrential downpours) and states fertility of topsoil in rainforest regions is very poor, linking heavy rainfall to nutrient loss.
A student could combine heavy-rain leaching with rapid decomposition (nutrients released but then leached) to evaluate whether net soil nutrient levels are high or low.
An objective question option identifies tropical laterite soil as 'too infertile' as a reason for sparse undergrowth, suggesting a pattern of low soil fertility in equatorial forests.
A student could use this as an example that despite dense vegetation, soil infertility is common in equatorial climates and investigate mechanisms (decomposition + leaching) that explain it.
Describes tropical rain forests as occurring near the equator with high and uniform temperature and humidity and notes soils are red latosols (a characteristic tropical soil).
Using the climate description plus knowledge that latosols are often heavily weathered, a student could link climate-driven decomposition/weathering to likely low retained soil nutrients.
- [THE VERDICT]: Sitter. Directly lifted from NCERT Class XI (Fundamentals of Physical Geography, Ch: Geomorphic Processes/Soils) and Majid Hussain (Biomes).
- [THE CONCEPTUAL TRIGGER]: The 'Nutrient Cycling' theme in Biogeography. Specifically, the relationship between Temperature, Moisture, and Bacterial Activity.
- [THE HORIZONTAL EXPANSION]: Contrast this with other biomes: Tundra (Low temp = Slow decomp = Peat accumulation); Grasslands (Moderate rain = High humus = Chernozems/Black Soil); Coniferous (Acidic needles = Podzolization). Memorize the soil types: Oxisols/Laterites (Tropics) vs. Spodosols (Taiga).
- [THE STRATEGIC METACOGNITION]: Do not study biomes as static lists of trees. Study them as 'Chemical Reactors'. Ask: Where are the nutrients stored? In Rainforests, the bank is the Biomass (trees); in Grasslands, the bank is the Soil.
Tropical rain forests commonly develop red latosols (lateritic soils), which are the dominant soil type under these forests.
High-yield: explains why tropical vegetation is dense yet soils can be poor; links soil type to questions on land use, agriculture and forest conversion. Mastery helps answer questions about soil classification, fertility and sustainable farming in tropical regions.
- Environment, Shankar IAS Acedemy .(ed 10th) > Chapter 3: Terrestrial Ecosystems > 3.2.5. Tropical rain forests: > p. 25
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 30: Climatic Regions > Explanation: > p. 429
Heavy leaching in humid tropical climates removes soluble nutrients, producing soils with low inherent fertility and only short-lived gains after burning vegetation.
Crucial for questions on shifting cultivation, sustainability, and why cleared rain forest land fails after a few crops; connects climate (high rainfall) to pedogenesis and agricultural outcomes.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 30: Climatic Regions > Explanation: > p. 429
- Environment, Shankar IAS Acedemy .(ed 10th) > Chapter 1: Ecology > r.3.6. Biosphere > p. 10
Tropical rain forests are extremely diverse and productive aboveground while the soils remain heavily leached and of low fertility.
Useful for explaining the apparent paradox in ecology and geography papers: why biomass and biodiversity can be high even when soil nutrients are low; links to nutrient cycling and ecosystem services questions.
- Environment, Shankar IAS Acedemy .(ed 10th) > Chapter 3: Terrestrial Ecosystems > 3.2.5. Tropical rain forests: > p. 25
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 30: Climatic Regions > Explanation: > p. 429
High temperature combined with abundant moisture accelerates bacterial growth and the breakdown of dead plant material in tropical rainforests.
High-yield concept for questions on nutrient cycling, soil fertility and biome functioning; connects microbiology of decomposition with land‑use outcomes (e.g., short-lived fertility after forest clearing). Mastering this helps answer comparative questions on soils across climates and on post-deforestation agriculture.
- Environment and Ecology, Majid Hussain (Access publishing 3rd ed.) > Chapter 3: MAJOR BIOMES > 1. Tropical Evergreen Rainforest Biome > p. 5
- FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 5: Geomorphic Processes > Biological Activity > p. 45
- Environment and Ecology, Majid Hussain (Access publishing 3rd ed.) > Chapter 1: BASIC CONCEPTS OF ENVIRONMENT AND ECOLOGY > Decomposers or Saprophytes > p. 31
Rapid decomposition and immediate root uptake prevent accumulation of organic matter, leaving rainforest soils low in humus despite high productivity.
Essential for explaining why tropical forests often produce poor soils for sustained agriculture, for linking vegetation productivity with soil profiles (laterites), and for answering questions about conservation and land management after deforestation.
- Environment and Ecology, Majid Hussain (Access publishing 3rd ed.) > Chapter 3: MAJOR BIOMES > 1. Tropical Evergreen Rainforest Biome > p. 5
- FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 5: Geomorphic Processes > Biological Activity > p. 45
Equatorial climates lack a dormant season, so decay processes operate continuously rather than seasonally, increasing turnover of organic matter.
Useful for comparing biomes (tropical vs temperate/tundra), understanding peat formation absence in tropics, and tackling questions on seasonal vs perennial ecosystem processes.
- Physical Geography by PMF IAS, Manjunath Thamminidi, PMF IAS (1st ed.) > Chapter 30: Climatic Regions > Equatorial Vegetation > p. 426
- Environment and Ecology, Majid Hussain (Access publishing 3rd ed.) > Chapter 3: MAJOR BIOMES > 1. Tropical Evergreen Rainforest Biome > p. 5
High temperature and moisture accelerate microbial decomposition, resulting in low humus accumulation in tropical soils.
Explaining contrasts in soil organic matter across climates is high-yield for geography and environment questions; it links microbial activity to soil fertility and helps answer questions on biome-specific soil properties and land-use implications.
- Environment and Ecology, Majid Hussain (Access publishing 3rd ed.) > Chapter 3: MAJOR BIOMES > 1. Tropical Evergreen Rainforest Biome > p. 5
- FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 5: Geomorphic Processes > Biological Activity > p. 45
Since they asked about rapid decomposition in Tropics, the next logical question is the exact opposite: 'Peat Formation' in Tundra/Boreal regions. Because of low temperatures, bacterial activity is inhibited, leading to massive carbon storage in soil (Peat) rather than biomass. Also, look out for 'Blue Carbon' (Mangroves/Seagrass) which stores carbon in anaerobic soil conditions.
Use the 'Stock vs. Flow' Logic. If Statement II is true (decomposition is fast due to heat/moisture), then nutrients are being released and used up rapidly (High Flow). If the flow is super fast, the stock (Statement I: Soil richness) cannot be high. The two statements are functionally contradictory. Since high heat/moisture undeniably speeds up chemical reactions (Science 101), Statement II is the anchor truth, making Statement I false.
Mains GS-3 (Agriculture & Environment): This concept explains why 'Shifting Cultivation' (Jhum) fails if the fallow period is too short. Once the vegetation (the nutrient bank) is burnt and crops are grown, the soil (which is inherently poor) loses fertility within 2-3 cycles. This is the scientific basis for arguing against slash-and-burn in high-density populations.