What structural and chemical properties make chernozems highly fertile?

Excellent structure with good drainage and water retention, high natural fertility, and neutral to slightly alkaline pH.

Where are chernozem soils distributed globally?

In mid-latitude continental interiors with temperate grassland vegetation, including the Ukrainian steppes, North American prairies, and Argentine pampas.

What type of agriculture do chernozems typically support?

Large-scale commercial grain production, particularly wheat and maize.

Why are chernozem regions important for global food supply?

Chernozems are among the world's most productive agricultural soils, producing large grain surpluses that are exported to feed populations elsewhere.

AQA A-Level Geography 7037

Water and Carbon Cycles

Topic overview Systems, Stores and Flows Mass Balance in Water and Carbon Stores Fieldwork and the Rainforest Case Study Measures of Central Tendency and Dispersion Spearman's Rank, Chi-Square and Data Analysis Scatter Graphs, Triangular Graphs and Logarithmic Scales Atlas, Thematic and Flow-Line Maps OS Maps, Sketch Maps and Field Sketches Remote Sensing, GIS and Big Data Qualitative Data, Questionnaires and Interviews Sampling, Accuracy and Measurement Error Data Misuse and Research Ethics The Global Water Stores Evaporation, Condensation and Cloud Formation Precipitation and Cryospheric Processes The Drainage Basin as an Open System Infiltration and Overland Flow The Water Balance Equation Flood Hydrographs Human Impacts on the Water Cycle The Global Carbon Stores Photosynthesis, Respiration and Carbon Transfer Farming, Land Use and Carbon Sinks Greenhouse Gases and Links between the Cycles Feedback Loops and Climate Change Carbon Sequestration and Mitigation Mass Balance in a Drainage Basin Unit Conversion and Flux Calculations Line Graphs, Bar Graphs and Pie Charts Water and Carbon Cycles in the Tropical Rainforest The Amazon rainforest case study Stores within a River Catchment Transfers and the Controls on Catchment Hydrology The River Eden catchment case study

Hot Desert Systems and LandscapesLandscape

Topic overview Deserts as Systems: Inputs, Stores, Flows and Feedback Desert Climate, Soils and Vegetation The Aridity Index Energy, Sediment and Geomorphic Processes in Deserts Thermal Fracture and Rock Breakdown Deflation, Abrasion and Aeolian Transport Desert Water Sources and Ephemeral Streams Deflation Hollows, Yardangs and Zeugen Barchan and Seif Dunes Wadis, Bahadas and Pediments Playas, Inselbergs and Landscape Development Observation, Measurement and Mapping in Deserts Death Valley hot desert case study The Causes and Definition of Desertification Environmental Impacts of Desertification Human Impacts and Responses to Desertification Desertification on the Yatenga plateau, Burkina Faso

Coastal Systems and LandscapesLandscape

Topic overview Energy Inputs to the Coastal System Coastal Flows and Feedback Waves, Tides and Sediment Cells Marine Erosion and Transport Processes Cliffs, Notches and Wave-Cut Platforms Beaches, Spits and Bars Sand Dune Formation and Succession Estuaries, Mudflats and Saltmarsh Sea Level Change and Coastlines of Submergence Emergent Coastlines and Present Sea Level Rise Hard Engineering at the Coast Soft Engineering and Managed Retreat The Holderness coast case study The Sundarbans and the Ganges–Brahmaputra delta

Glacial Systems and LandscapesLandscape

Topic overview Glaciers as Systems: Inputs, Stores and Flows Ice-Albedo and Negative Feedback Dynamic Equilibrium, Landforms and Landscapes The Glacial Mass Budget and Ice Movement The Distribution of Cold Environments Climate, Soils and Vegetation in Cold Environments Corrie Formation Glacial Troughs and Hanging Valleys Roches Moutonnées, Drumlins and Erratics Moraines, Till and Fluvioglacial Landforms Periglacial Landforms and Processes Thermokarst and Landform Distribution The Fragility of Cold Environments Impacts and Management of Cold Environments Fieldwork Skills in Glaciated Environments Glacial Case Study Requirements Cwm Idwal and the Ogwen valley case study Alaska as a contrasting glaciated landscape

HazardsHazards or ecosystems

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Ecosystems Under StressHazards or ecosystems

Topic overview Biodiversity Levels and Causes of Decline Biodiversity Loss and Ecosystem Services Ecosystem Structure, Trophic Levels and Food Webs Ecosystem Inputs, Outputs, Stores and Transfers Biomass, Net Primary Production and Succession Nutrient Cycling, Climate and Soil Environmental Controls and Ecosystem Feedback Biomes and the Tropical Rainforest Environment Rainforest Stratification and Adaptations Savanna Climate, Soils and Adaptations Human Impacts on the Tropical Rainforest Human Impacts on the Savanna Succession and Climatic Climax Temperate Deciduous Woodland Plagioclimax and Heather Moorland Coral Reef Conditions, Services and Stresses Human Pressures and Coral Reef Management The Great Barrier Reef: Extent and Bleaching Crown-of-Thorns Starfish and Reef Tourism Local Ecosystems: Heathland, Parkland, Ponds and Dunes Adaptations to Dry Environments Agriculture, Urbanisation and Invasive Species Ecological Change and Conservation Strategies Sustainability and Stakeholder Conflict Studying Local Ecosystems and Ecological Change The Sefton Coast sand dunes case study Ecological change in Borneo

Global Systems and Global Governance

Changing Places

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Contemporary Urban EnvironmentsHuman option

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Population and the EnvironmentHuman option

Topic overview The Physical Environment and Population Global Food Production and Agricultural Systems Tropical Wet and Semi-Arid Climates Zonal Soils: Chernozems and Latosols Soil Erosion and Its Management Waterlogging, Salinisation and Soil Structure The Dimensions of Food Security Studying Climatic Types and Zonal Soils Glasgow: place and health case study Health, Morbidity and the Epidemiological Transition Physical Environment and Disease Malaria: Distribution, Impacts and Management Coronary Heart Disease and Non-Communicable Diseases Global Health Initiatives and Disease Studies The Demographic Transition Model Fertility, Population Structure and the Demographic Dividend Migrant Types and Causes of Migration Push and Pull Factors in Migration The Components of Population Change Optimum Population and Resource Demand Ecological Footprint and Population–Resource Theories Ozone Depletion and Human Health Climate Change, Heatwaves and Vector-Borne Disease Climate Change, Food Supply and Nutrition Global Population Projections Japan's population decline

Resource SecurityHuman option

Topic overview Stock and Flow Resources and Reserves Resource Certainty and Development Stages Resource Frontiers, Peaks and Sustainable Development Environmental Impact Assessment Global Production and Consumption of Energy and Minerals The Geopolitics of Energy, Minerals and Water Water Sources and Demand Water Supply Strategies The Colorado River water supply scheme The Costs of Supply and Managing Demand Water Conflict and Major Supply Schemes Energy Types, Mix and Physical Controls on Supply TNCs, National Interests and Energy Impacts Increasing Energy Supply: Unconventional, Nuclear and Renewable Reducing Energy Demand Environmental Impacts and Sustainability of Energy The Alberta oil sands development Choosing a Mineral Ore Case Study Demand for and Occurrence of Mineral Ores The Environmental Cost of Mineral Extraction The Bingham Canyon copper mine Sustainability in Mineral Supply Alternative Energy Futures Alternative Water Futures Mineral Ore Futures Drivers of Resource Transitions Resource Security and Human Welfare

Population and the Environment

Zonal Soils: Chernozems and Latosols

2 things to know
Component 2

Overview

Recall questions on the A horizon, fertility, distribution and farming of chernozems and their importance for food supply, and on the colour, low fertility and distribution of latosols, shifting cultivation and what permanent cultivation on them requires.

What you need to know

Answer each one before you reveal it.

Your recallNot started

Key term

Describe the A horizon characteristics of chernozem soils.

Key term

What gives latosols their characteristic red or yellow colour?

Questions from this subtopic

Each one with the model answer underneath.

1
Describe the A horizon characteristics of chernozem soils.
Model answer
Chernozems have a deep, dark A horizon rich in humus organic matter.
2
What structural and chemical properties make chernozems highly fertile?
Model answer
Excellent structure with good drainage and water retention, high natural fertility, and neutral to slightly alkaline pH.
3
Where are chernozem soils distributed globally?
Model answer
In mid-latitude continental interiors with temperate grassland vegetation, including the Ukrainian steppes, North American prairies, and Argentine pampas.
4
What type of agriculture do chernozems typically support?
Model answer
Large-scale commercial grain production, particularly wheat and maize.
5
Why are chernozem regions important for global food supply?
Model answer
Chernozems are among the world's most productive agricultural soils, producing large grain surpluses that are exported to feed populations elsewhere.
6
What gives latosols their characteristic red or yellow colour?
Model answer
Iron and aluminium oxides resulting from deep weathering processes.

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AThe horns have less sand volume, so they move more quickly.

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