Practice
Dryland Farming
Also known as: dry farming, rainfed agriculture in arid regions
A family of agricultural practices that grow crops without irrigation in regions with low or unreliable rainfall — typically under 500 mm/year. Relies on tillage and mulch techniques to capture and conserve every drop of seasonal rain in the soil profile, drought-tolerant crop varieties, wide row spacing, and fallow rotations that bank moisture for the next season. The traditional agriculture of much of the world's grain belt and a critical practice as freshwater aquifers decline.
Practical
The dryland farmer’s central problem: how to grow a crop on rainfall that arrives in unpredictable bursts and is lost quickly to runoff and evaporation. Traditional and modern answers:
- Stubble-mulch fallow — leave previous crop’s residue on the surface during the off-season; reduces evaporation, slows runoff.
- Wide row spacing — fewer plants per area means each plant has access to more soil moisture.
- Drought-tolerant varieties — long taproots, waxy leaf cuticles, deep root systems, short cycles. Many indigenous crops (Hopi corn, Diné peach, Mediterranean wheat landraces) are dryland-adapted by centuries of selection.
- [[no-till-farming|No-till]] or minimum-till — preserves soil structure and organic matter; tillage breaks capillary continuity that brings water to the root zone.
- [[cover-cropping|Cover cropping]] in winter — captures off-season rainfall; living roots maintain mycorrhizal infrastructure.
- Crop-fallow rotation — alternating years of crop and fallow lets [[soil|the soil]] bank moisture for the cropping year.
Scientific
The dryland water-use efficiency frontier is set by transpiration biology — the C4 grasses (corn, [[sorghum|sorghum]], millet) and the deep-rooted legumes have inherent advantages over C3 crops in low-rainfall environments. [[plant-breeding|Plant breeding]] for drought tolerance has been substantial over the past century, but the largest gains in dryland productivity come from soil-water management — keeping rainfall in the soil long enough for the crop to use it.
[[wes-jackson|Wes Jackson]]‘s perennial-grain work at The Land Institute is, in significant part, a dryland-farming program: deep-rooted perennial polycultures designed to thrive in the tallgrass-prairie rainfall regime that dryland wheat-and-fallow systems struggle in.
Cultural
Dryland farming is the backbone of food production across the U.S. Great Plains, the Mediterranean basin, the Indian Deccan plateau, the African Sahel, the Australian wheat belt, and the Andean altiplano. Industrial-irrigation agriculture is a 20th-century phenomenon that depends on aquifer water-banks ([[ogallala-aquifer|Ogallala]], Central Valley) that are now visibly drawing down. Dryland practice will be the long-term default again, on more land and more soon than U.S. agricultural policy currently assumes.
Lenses still to grow
- The [[ogallala-aquifer|Ogallala aquifer]] drawdown and the dryland-farming question for the U.S. Great Plains
- Indigenous Southwest dryland agriculture (Hopi, Pueblo, Tohono O’odham systems)
- The Mediterranean dryland tradition (olives, wine grapes, durum wheat, pulses)
- Modern dryland-farming research stations (CIMMYT, ICRISAT, USDA-ARS)
See also
Auto-generated from this entry’s typed relations: frontmatter, grouped by relation type so the editorial signal isn’t flattened.
- Enables: [[heritage-corn]]
- Shares approach with: [[cover-cropping]]
- Counterpart to: [[rainwater-harvesting]]
- Member of: [[practice]]
Sources
- [[wes-jackson|Wes Jackson]], New Roots for Agriculture
- David Montgomery, Growing a Revolution (chapter on dryland transitions)
- USDA-ARS Conservation Research dryland publications
- [[gary-paul-nabhan|Gary Paul Nabhan]], Growing Food in a Hotter, Drier Land
Rooted in life.
What links here, and how
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Practical
opposes
- Groundwater Depletion dryland farming is the structural alternative to irrigation-based agriculture on aquifer water; the long-term default for the Great Plains will be dryland or non-cropping
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