Soil Infiltration Rate Calculator
ANA›Life Services Authority›National Calculator Authority›Soil Infiltration Rate Calculator
.calc-container { max-width: 640px; margin: 2rem 0; padding: 1.5rem; background: #fff; border: 1px solid #ddd; border-radius: 8px; box-shadow: 0 1px 3px rgba(0,0,0,0.06); font-family: system-ui, -apple-system, sans-serif; } .calc-container h3 { font-family: Georgia, serif; font-size: 1.15rem; color: #1a1a1a; margin-bottom: 1rem; padding-bottom: 0.5rem; border-bottom: 2px solid var(--ac, #3d5a80); } .calc-row { display: flex; align-items: center; gap: 0.75rem; margin-bottom: 0.75rem; flex-wrap: wrap; } .calc-row label { min-width: 160px; font-size: 0.9rem; color: #333; font-weight: 500; } .calc-row input[type="number"], .calc-row select { flex: 1; min-width: 120px; max-width: 200px; padding: 0.5rem 0.6rem; border: 1px solid #ccc; border-radius: 4px; font-size: 0.9rem; font-family: system-ui, sans-serif; color: #1a1a1a; background: #fafaf8; } .calc-row input:focus, .calc-row select:focus { outline: none; border-color: var(--ac, #3d5a80); box-shadow: 0 0 0 2px rgba(26,74,138,0.12); } .calc-row .unit { font-size: 0.82rem; color: #888; min-width: 30px; } .calc-btn { display: inline-block; margin-top: 0.5rem; padding: 0.55rem 1.5rem; background: var(--ac, #3d5a80); color: #fff; border: none; border-radius: 4px; font-size: 0.9rem; font-weight: 600; cursor: pointer; font-family: system-ui, sans-serif; } .calc-btn:hover { opacity: 0.9; } .calc-result { margin-top: 1.25rem; padding: 1rem 1.25rem; background: #f0f6fc; border-left: 3px solid var(--ac, #3d5a80); border-radius: 0 6px 6px 0; display: none; } .calc-result.visible { display: block; } .calc-result-label { font-size: 0.78rem; text-transform: uppercase; letter-spacing: 0.06em; color: #666; margin-bottom: 0.25rem; } .calc-result-value { font-size: 1.6rem; font-weight: 700; color: var(--ac, #3d5a80); } .calc-result-detail { font-size: 0.85rem; color: #555; margin-top: 0.5rem; line-height: 1.5; } .calc-note { margin-top: 1rem; font-size: 0.8rem; color: #888; font-style: italic; } .calc-grid { display: grid; grid-template-columns: 1fr 1fr; gap: 0.75rem; margin-top: 0.75rem; } .calc-grid-item { padding: 0.6rem 0.8rem; background: #f8f9fa; border-radius: 4px; border: 1px solid #eee; } .calc-grid-item .label { font-size: 0.75rem; color: #888; text-transform: uppercase; letter-spacing: 0.04em; } .calc-grid-item .value { font-size: 1.1rem; font-weight: 600; color: #1a1a1a; } @media (max-width: 720px) { .calc-row { flex-direction: column; align-items: flex-start; gap: 0.3rem; } .calc-row label { min-width: auto; } .calc-row input[type="number"], .calc-row select { max-width: 100%; width: 100%; } .calc-grid { grid-template-columns: 1fr; } } .calc-chart { margin: 1rem 0; text-align: center; } .calc-chart svg { max-width: 100%; height: auto; } .calc-chart-legend { display: flex; flex-wrap: wrap; justify-content: center; gap: 0.6rem 1.2rem; margin-top: 0.6rem; font-size: 0.8rem; color: #555; } .calc-chart-legend span { display: inline-flex; align-items: center; gap: 0.3rem; } .calc-chart-legend i { display: inline-block; width: 10px; height: 10px; border-radius: 2px; font-style: normal; } .calc-related { max-width: 640px; margin: 2rem 0 1rem; padding: 1.25rem 1.5rem; background: #f8f9fa; border: 1px solid #e8e8e8; border-radius: 8px; } .calc-related h3 { font-family: Georgia, serif; font-size: 1rem; color: #1a1a1a; margin: 0 0 0.75rem; padding-bottom: 0.4rem; border-bottom: 2px solid var(--ac, #3d5a80); } .calc-related-list { list-style: none; padding: 0; margin: 0 0 0.75rem; display: grid; grid-template-columns: 1fr 1fr; gap: 0.4rem 1.5rem; } .calc-related-list li a { font-size: 0.88rem; color: var(--ac, #3d5a80); text-decoration: none; } .calc-related-list li a:hover { text-decoration: underline; } .calc-browse-all { margin: 0.5rem 0 0; font-size: 0.9rem; font-weight: 600; } .calc-browse-all a { color: var(--ac, #3d5a80); text-decoration: none; } .calc-browse-all a:hover { text-decoration: underline; } @media (max-width: 720px) { .calc-related-list { grid-template-columns: 1fr; } }
Soil Infiltration Rate Calculator
Calculate cumulative infiltration and infiltration rate using Philip's Two-Term Method or the Green-Ampt Method for various soil types.
Calculation Method
Philip's Two-Term Method Green-Ampt Method
Sorptivity, S (mm/hr^0.5)
Soil water absorption capacity (typical range: 5–100 mm/hr⁰·⁵)
Transmissivity Constant, A (mm/hr)
Steady-state transmission rate (typical range: 1–50 mm/hr)
Time, t (hours)
Elapsed time since infiltration began (must be > 0)
Soil Texture Class
Sand Loamy Sand Sandy Loam Loam Silt Loam Sandy Clay Loam Clay Loam Silty Clay Loam Sandy Clay Silty Clay Clay
Saturated Hydraulic Conductivity, K_s (mm/hr)
Auto-filled from soil type; can be overridden
Wetting Front Suction Head, ψ (mm)
Capillary suction at wetting front; auto-filled from soil type
Effective Porosity, θ_e (dimensionless)
Fraction of soil volume available for water (0–1); auto-filled
Initial Soil Moisture Content, θ_i (dimensionless)
Volumetric water content before rainfall (must be
Time, t (hours)
Elapsed time since infiltration began (must be > 0)
Calculate Results will appear here.
// Green-Ampt soil parameters: [Ks (mm/hr), psi (mm), theta_e] // Source: Rawls, Brakensiek & Miller (1983); Chow, Maidment & Mays (1988) const soiSoilParams = { sand: [117.8, 49.5, 0.417], loamy_sand: [ 29.9, 61.3, 0.401], sandy_loam: [ 10.9, 110.1, 0.412], loam: [ 3.4, 88.9, 0.434], silt_loam: [ 6.5, 166.8, 0.486], sandy_clay_loam: [ 1.5, 218.5, 0.330], clay_loam: [ 1.0, 208.8, 0.390], silty_clay_loam: [ 1.0, 273.0, 0.432], sandy_clay: [ 0.6, 239.0, 0.321], silty_clay: [ 0.5, 292.2, 0.423], clay: [ 0.3, 316.3, 0.385] };
function soiToggleMethod() { const method = document.getElementById('soi-method').value; document.getElementById('soi-philip-inputs').style.display = (method === 'philip') ? '' : 'none'; document.getElementById('soi-greenampt-inputs').style.display = (method === 'greenampt') ? '' : 'none'; document.getElementById('soi-result').innerHTML = 'Results will appear here.'; }
function soiLoadSoilParams() { const type = document.getElementById('soi-soil-type').value; const p = soiSoilParams[type]; document.getElementById('soi-hydraulic-cond').value = p[0]; document.getElementById('soi-suction').value = p[1]; document.getElementById('soi-porosity').value = p[2]; }
// Load defaults on page load soiLoadSoilParams();
function soiCalc() { const method = document.getElementById('soi-method').value; const resultDiv = document.getElementById('soi-result');
if (method === 'philip') { const S = parseFloat(document.getElementById('soi-sorptivity').value); const A = parseFloat(document.getElementById('soi-transmissivity').value); const t = parseFloat(document.getElementById('soi-time-philip').value);
if (isNaN(S) || isNaN(A) || isNaN(t)) { resultDiv.innerHTML = '⚠ Please fill in all fields.'; return; } if (S ⚠ Sorptivity and Transmissivity must be ≥ 0.'; return; } if (t ⚠ Time must be greater than 0.'; return; }
// Philip's Two-Term Method // Cumulative infiltration: F(t) = S·t^0.5 + A·t [mm] // Infiltration rate: f(t) = 0.5·S·t^(-0.5) + A [mm/hr] const F = S * Math.pow(t, 0.5) + A * t; const f = 0.5 * S * Math.pow(t, -0.5) + A;
// Steady-state rate (as t → ∞, f → A) const f_steady = A;
resultDiv.innerHTML = ` ### Philip's Two-Term Method Results
ParameterValue Cumulative Infiltration, F(t)${F.toFixed(3)} mm Infiltration Rate, f(t)${f.toFixed(4)} mm/hr Steady-State Rate (t→∞)${f_steady.toFixed(4)} mm/hr Sorptivity, S${S.toFixed(3)} mm/hr⁰·⁵ Transmissivity Constant, A${A.toFixed(3)} mm/hr Time, t${t.toFixed(3)} hr `;
} else { // Green-Ampt Method const Ks = parseFloat(document.getElementById('soi-hydraulic-cond').value); const psi = parseFloat(document.getElementById('soi-suction').value); const te = parseFloat(document.getElementById('soi-porosity').value); const ti = parseFloat(document.getElementById('soi-initial-moisture').value); const t = parseFloat(document.getElementById('soi-time-ga').value);
if (isNaN(Ks) || isNaN(psi) || isNaN(te) || isNaN(ti) || isNaN(t)) { resultDiv.innerHTML = '⚠ Please fill in all fields.'; return; } if (Ks ⚠ Hydraulic conductivity must be > 0.'; return; } if (psi ⚠ Suction head must be ≥ 0.'; return; } if (te = 1) { resultDiv.innerHTML = '⚠ Effective porosity must be between 0 and 1.'; return; } if (ti = te) { resultDiv.innerHTML = '⚠ Initial moisture must be ≥ 0 and less than effective porosity.'; return; } if (t ⚠ Time must be greater than 0.'; return; }
// Moisture deficit (IMD = Initial Moisture Deficit) const IMD = te - ti;
// Green-Ampt cumulative infiltration (implicit equation solved iteratively): // F(t) = Ks·t + ψ·IMD·ln(1 + F(t)/(ψ·IMD)) // Solve using Newton-Raphson iteration const psiIMD = psi * IMD; let F = Ks * t; // initial guess const maxIter = 200; const tol = 1e-9;
for (let i = 0; i ParameterValue Cumulative Infiltration, F(t)${F.toFixed(3)} mm Infiltration Rate, f(t)${f.toFixed(4)} mm/hr Steady-State Rate (= K_s)${f_steady.toFixed(4)} mm/hr Initial Moisture Deficit (IMD)${IMD.toFixed(4)} ψ × IMD${psiIMD.toFixed(3)} mm Saturated Hydraulic Conductivity, K_s${Ks.toFixed(3)} mm/hr Wetting Front Suction, ψ${psi.toFixed(1)} mm Effective Porosity, θ_e${te.toFixed(3)} Initial Moisture, θ_i${ti.toFixed(3)} Time, t${t.toFixed(3)} hr `; } }
#### Formulas
Philip's Two-Term Method:
- Cumulative Infiltration: F(t) = S·t0.5 + A·t
- Infiltration Rate: f(t) = ½·S·t−0.5 + A
Where S = sorptivity (mm/hr⁰·⁵), A = transmissivity constant (mm/hr), t = time (hr).
Green-Ampt Method:
- Cumulative Infiltration (implicit): F(t) = Ks·t + ψ·IMD·ln(1 + F(t)/(ψ·IMD))
- Infiltration Rate: f(t) = Ks·(1 + ψ·IMD / F(t))
- Initial Moisture Deficit: IMD = θe − θi
Where Ks = saturated hydraulic conductivity (mm/hr), ψ = wetting front suction head (mm), θe = effective porosity, θi = initial moisture content. The implicit equation is solved via Newton-Raphson iteration.
#### Assumptions & References
- Green-Ampt soil parameters (Ks, ψ, θe) are mean values from Rawls, Brakensiek & Miller (1983) as tabulated in Chow, Maidment & Mays (1988).
- References: Philip, J.R. (1957). The theory of infiltration. Soil Science, 83(5), 345–357. | Green, W.H. & Ampt, G.A. (1911). Studies on soil physics. Journal of Agricultural Science, 4(1), 1–24. | Rawls, W.J., Brakensiek, D.L. & Miller, N. (1983). Green-Ampt infiltration parameters from soils data. ASCE Journal of Hydraulic Engineering, 109(1), 62–70.
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References
- Radon indoors source potential from soil gas in a temperate climate: impact of infiltration rate and seismicity. — Environ Sci Pollut Res Int (2024 Mar)
- Effects of soil bulk density and corresponding soil infiltration rate on the migration and transformation of gibberellic acid. — J Contam Hydrol (2025 Feb)
- Virus removal within a soil infiltration zone as affected by effluent composition, application rate, and soil type. — Water Res (2007 Feb)