Leaching Fraction
Also called: LF, Leaching Requirement, LR
Leaching fraction (LF) is the proportion of applied irrigation water that drains below the root zone to flush accumulated salts out of reach of crops. The Richards 1954 / FAO DP29 formula for steady-state irrigation: LF = ECiw / (5 × ECe_threshold − ECiw). Practical leaching fractions range from ~0.05 (low-salinity water + tolerant crop) to ~0.30 (saline water + sensitive crop); above 0.30, the operation is approaching uneconomical.
How Leaching Fraction Works
Salt accumulation in irrigated soils is unavoidable because every irrigation event delivers dissolved salts but only the water evaporates or transpires — the salts stay behind. Without periodic leaching, EC in the root zone rises until yields collapse. The leaching fraction tells you how much *extra* water (beyond crop ETc) you must apply so the salt stays diluted enough not to harm the next crop.
Worked example for olive (ECe threshold 4.0 dS/m) irrigated with EC 4.0 dS/m water: LF = 4 / (5 × 4 − 4) = 0.25. Gross irrigation = ETc × (1 + 0.25) — for an ETc of 5 mm/day during peak season, gross = 6.25 mm/day, with 1.25 mm draining as leachate. For Siwi date palm (threshold 8.0) on the same water: LF = 4 / (5 × 8 − 4) = 0.11 — a much smaller penalty, demonstrating why salt-tolerant crops are economically critical in saline regions.
Delivery strategy matters: under sprinkler or flood, leaching is naturally distributed because each event soaks the whole root zone. Under drip, salts accumulate at the wetting-front edge between emitters, so periodic deep watering (deficit irrigation cycle followed by a heavy leaching set every 2–4 weeks) outperforms continuous drip during high-EC seasons. Acid-flush of drip lines monthly above EC 2.0 dS/m prevents bicarbonate-precipitation clogging that otherwise reduces emitter uniformity and concentrates salts at remaining functional outlets. WiseYield's irrigation advisor reads the latest water-EC sample, computes the per-crop LF, increases the recommended gross irrigation accordingly, and surfaces a salt-clogging tip when EC exceeds the drip-clogging threshold.
Sources
- Richards, L.A. ed. (1954). Diagnosis and improvement of saline and alkali soils. USDA Agriculture Handbook 60.
- Ayers, R.S. & Westcot, D.W. (1985). Water quality for agriculture. FAO Irrigation and Drainage Paper No. 29 Rev. 1.
- Hoffman, G.J. & van Genuchten, M.Th. (1983). Soil properties and efficient water use: Water management for salinity control.