1001Ferramentas
💧 Calculators

Irrigation Flow Calculator

Calculate irrigation flow in L/h and mm/h from irrigated area, dripper count and unit flow. Useful for agricultural hydraulic projects.

Irrigation flow rate: sizing water demand

Flow rate per hectare comes from Q (L/h) = ETc · area / efficiency. Here ETc is the crop evapotranspiration in mm/day, the area is in m², and efficiency is the system's loss factor. In Brazil, ETc tends to sit near 5 mm/day through summer for most annual crops. Efficiency depends heavily on the method you pick. A center pivot runs 70–80%, a conventional sprinkler 65–75%, and drip irrigation clears 90%. Take 1 ha (10,000 m²) with ETc = 5 mm/day on an 80% pivot: that works out to 50,000 L/day / 0.8 = 62,500 L/day. Switch to localized drip and the number drops about 15%, since you lose nothing to wind drift or evaporation off wet soil.

Applications

It shows up in precision agriculture work, EMBRAPA water-management guidance, and water-grant requests filed under Lei 9.433/1997 (Política Nacional de Recursos Hídricos). Engineers also lean on it to size pumps and pipes, and to lay out the irrigation schedule once the dry season hits.

FAQ

How do I measure ETc? Take the reference evapotranspiration (ET0, pulled from a weather station) and multiply it by the crop coefficient (Kc). Kc shifts as the plant moves through its growth stages.

Why does drip beat pivot? Because it puts water right at the root zone, where almost nothing is lost to evaporation or wind. That pushes the effective fraction up toward 95%.

Do I need a water grant? In Brazil, once a catchment goes past the state's insignificant-use threshold (usually around 1 L/s), you need an outorga from ANA or the state water agency.

Related Tools

🌧️

Sprinkler Nozzle Flow

Compute sprinkler nozzle flow Q given pressure and discharge coefficient Cd. Q = Cd × A × √(2gh).

💧

Garden Watering Time Liters

Calculates watering time to deliver a target amount of liters given a flow rate.

💨

Plastic Injection Flow Rate

Compute the injection flow rate by dividing the injected volume by the fill time, in cm³/s. It is the speed at which the molten plastic enters the mold — a parameter that controls the shear rate, molecular orientation, surface finish and defects such as jetting or flow marks. High flow fills fast but may degrade; low flow may solidify before filling. Enter the injected volume and the fill time.

🚰

Geocomposite Drain Flow

Calculate the drainage flow of a drainage geocomposite, q = θ·i·b, from the transmissivity θ (m²/s), the hydraulic gradient i (dimensionless) and the drain width b (m). This is the practical application of transmissivity: it estimates how much water a drainage geocomposite (geonet between geotextiles, or drainage geotextile) can convey in its plane, to check whether it adequately replaces a gravel layer or conventional drain. The flow is the product of transmissivity (the drain's in-plane 'conductivity' at the work's confining pressure), the hydraulic gradient (the head-line slope driving the flow) and the drain width (the drainage front). It is Darcy's law applied to in-plane flow in the geosynthetic. This calculation is essential to size drainage systems with geocomposites: gas and liquid drainage in landfills and mining, drains behind walls and cutoffs, green-roof and buried-structure drainage, and road and railway drains. The flow the geocomposite provides is compared with the design flow (the water to drain, with a safety factor); if insufficient, a higher-transmissivity geocomposite is chosen or the width increased. Enter the transmissivity, hydraulic gradient and width.

🏗️

Solids Mass Flow (Dredge)

Calculate the mass flow of solids transported by a dredge or pipeline, ṁ_s = Q·C_v·ρ_s, from the total slurry flow Q (m³/s), the solids volumetric concentration C_v (fraction) and the solids density ρ_s (kg/m³). Solids mass flow is the MASS of useful material transported per unit time (kg/s, or tonnes per hour), the production indicator used when TONNAGE matters — the typical case of ore transport by pipeline (measured in t/h of dry ore) and mineral processing. It is the product of three factors: the slurry flow (pump capacity), the solids concentration (how 'loaded' the slurry is) and the solids density (iron ores, for example, are very dense, ~5000 kg/m³, so little volumetric concentration already gives high tonnage). Mass flow, integrated over time, gives the total transported tonnage, the basis of billing and operational mass balance. Optimizing it — maximizing tonnage per unit pumping energy — is the central goal of pipeline operation, which moves hundreds of millions of tonnes of ore per year over long distances far more energy-efficiently than trucks or trains. Enter the slurry flow, the volumetric concentration and the solids density.

🪣

Class A Pan Evaporation Calculator

Estimates reference evapotranspiration ETo in mm/day applying the Class A pan coefficient Kp to a measured evaporation.

The results provided by this tool are for general informational and educational purposes only and do not constitute professional, financial, medical, legal, tax or accounting advice. Always confirm important decisions with a qualified professional and official sources.