# Neighbour’s Runoff Flooding Your Lower Property in Grasse > Neighbor's runoff flooding your Grasse property? Prove the ditch is undersized with a Manning flow calculation and win your case. Call 04 22 46 06 04 - URL : https://cassini-expertise.fr/en/grasse-neighbor-runoff-manning-flow/ - Langue : en-US - Mis à jour : 2026-10-17 - Site : Cassini Expertise (https://cassini-expertise.fr/) NEIGHBOUR DISPUTES – WATER You come home after a storm in [Grasse](https://cassini-expertise.fr/grasse-secheresse-argile-fissures-donnees-officielles/) to find 15 cm of muddy water sitting in your garden, which lies lower than the land next door. Your neighbour’s property, higher up the slope, was regraded last year. Ever since, every time it rains, your land turns into a basin. You measured the ditch they dug: 80 cm wide. But is that enough to carry the water away? The answer lies in a calculation few property owners know about: the Manning-Strickler formula. ## What You See – And What It Actually Hides ![neighbor runoff water lower property grasse manning flow calculation - Cassini Expertise](https://cassini-expertise.fr/wp-content/uploads/2026/09/avant-achat-maison.webp) *Cassini Expertise – independent building expert* You see standing water. You suspect the neighbour. What no one tells you: Article 640 of the French Civil Code prohibits altering the natural flow of runoff water to the detriment of lower-lying land. But “detriment” can be measured. Field experience often shows a ditch sized purely “by eye.” In practice, what does that mean? A ditch that’s too small overflows every time. A ditch that’s too wide can be challenged as encroachment. You need the right number. Neighbour’s land (upslope) Slope I = 8% Your land (downslope) Flood zone Ditch Flow Q Width b = 0.80 m Height h = 0.40 m ## The Manning-Strickler Calculation That Changes Everything The formula is Q = K × R^(2/3) × I^(1/2) × S. Q is the flow rate (m³/s). K is the roughness coefficient (bare earth: 20). R is the hydraulic radius. I is the slope. S is the wetted cross-section. Let’s use realistic figures for Grasse, with its pronounced slopes. The ditch is 0.80 m wide (b) and holds 0.40 m of water depth (h) during a storm. Cross-section S = b × h = 0.80 × 0.40 = 0.32 m². Wetted perimeter P = b + 2h = 0.80 + 0.80 = 1.60 m. Hydraulic radius R = S / P = 0.32 / 1.60 = 0.20 m. Slope I = 8% (0.08) – typical of the Grasse hillsides. Now the calculation: Q = 20 × (0.20)^(2/3) × (0.08)^(1/2) × 0.32. (0.20)^(2/3) ≈ 0.34. (0.08)^(1/2) ≈ 0.283. So Q = 20 × 0.34 × 0.283 × 0.32 ≈ 0.616 m³/s – that’s 616 litres per second. Standard NF EN 12056-3 (section 4.2.1) requires a ditch of this kind to be sized for a ten-year storm event. In Grasse, ten-year rainfall intensity is around 90 mm/h. For an upstream surface of 800 m² (the neighbour’s land), the inflow is: (90/1000/3600) × 800 ≈ 0.020 m³/s (20 L/s). The ditch can theoretically carry 616 L/s – more than enough. But if the actual water depth h is only 0.15 m (a poorly maintained ditch), Q drops to 0.155 m³/s. And if the slope is only 3% (after regrading), Q = 0.112 m³/s. What this means in practice: a poorly sized or silted-up ditch in Grasse can be undersized by a factor of 5 relative to what’s needed. Your flooding has a measurable technical cause. ## What Happens If You Do Nothing Within 6 months, erosion will carve channels into your land. Your trees’ roots, starved of oxygen, will start showing signs of rot. Within 2 years, repeated water stagnation will change the soil’s bearing capacity. You’ll start seeing localised subsidence near the property line. One client in Grasse watched their fence tilt 10 cm over 18 months because of exactly this. And frankly, the cost? Stabilising an eroded slope and draining a 1,000 m² plot in Grasse runs between €8,000 and €15,000. That’s before counting secondary damage: rising damp reaching the house, mould developing on buried walls, foundation degradation if water sits against them. This isn’t just a puddle – it’s an accelerating process of deterioration. ## Remedies and Guarantees: What You Can Demand Article 640 of the Civil Code is your guarantee. It requires the owner of the higher-lying land not to worsen the natural water flow. If the Manning calculation proves the development has created excess flow or abnormal stagnation, you’re entitled to demand restoration. The process: send a formal notice by registered letter, including a preliminary calculation. If the neighbour disputes it, have a construction/land-surveying expert carry out a survey using a total station (±1 cm precision) to measure the actual slope and elevations. The Grasse Judicial Court has jurisdiction. What we always tell clients: a number beats an argument. Here, the key figure is the flow rate Q. If it exceeds the predictable natural flow (calculated from Grasse rainfall data), you’ll win your case. ## Frequently Asked Questions ### My neighbour changed how rainwater flows and my land is flooded – what should I do? Article 640 of the French Civil Code prohibits altering the natural flow of water to the detriment of lower-lying land. Have an expert (such as a land-surveying expert or hydraulic engineer) document the poor drainage and any undersizing of the ditch. Send your neighbour a formal notice, then take the matter to the judicial court if needed. A Manning-Strickler calculation lets you measure the flow precisely and prove the damage. ### How much does an expert assessment cost for a runoff water dispute between neighbours in Grasse? A technical assessment to size a ditch or analyse water flow is quoted free within 24 hours depending on complexity. This includes topographic surveys, flow calculations (Manning-Strickler), and a report usable in court. The timeframe is generally 2 to 4 weeks. This cost can often be recovered if you win your case. ### How do you calculate runoff water flow using the Manning-Strickler formula? The formula is Q = K × R^(2/3) × I^(1/2) × S. K is the roughness coefficient (20 for bare earth), R is the hydraulic radius (wetted cross-section divided by wetted perimeter), I is the slope in m/m, and S is the wetted cross-section. For a ditch 0.80 m wide with 0.40 m of water depth and an 8% slope, the flow is roughly 0.616 m³/s (616 L/s). Adjust the values to match your own situation. ### What’s the standard for sizing a stormwater drainage ditch? Standard NF EN 12056-3 requires ditches to be sized for a ten-year storm event. In Grasse, ten-year rainfall intensity is around 90 mm/h. For an 800 m² catchment area, the inflow is 0.020 m³/s (20 L/s). A properly sized ditch must be able to carry at least this flow. If your ditch is silted up or too small, it can be undersized by a factor of 5. ### What if my land is lower than my neighbour’s and their water keeps pooling on my property? Start by measuring the width and depth of your neighbour’s ditch, as well as its slope. Use the Manning formula to check whether the flow capacity is sufficient. If the ditch is undersized, ask your neighbour to enlarge or clear it. If they refuse, bring in an expert and pursue a claim for abnormal neighbourhood nuisance. Don’t wait: standing water can damage your land through erosion, root suffocation, and ground subsidence. **Need an expert?** See our dedicated page: Land Disputes and Boundary Expertise – response within 24 hours across the Alpes-Maritimes and Var. **See also:** [Water Drainage Easement Dispute in Antibes: Calculating the Flow Rate](https://cassini-expertise.fr/en/water-drainage-easement-flow-rate-dispute-antibes/) 📅 **Updated on 18/08/2026** – By **Cassini Expertise**, independent building expert covering départements 06, 83 & 13. Free quote: [04 22 46 06 04](tel:+33422460604). --- Source : https://cassini-expertise.fr/en/grasse-neighbor-runoff-manning-flow/