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Field guide · Drought resilience

Lost 30% of your harvest in two dry years? What to do to the soil, not the irrigation

The 30% is your figure, not ours, and no one can promise to give a defined share of it back. After two dry years the deficit usually sits in what the soil stores and what the roots reach, not in the pipework: irrigation moves water, it does not make a soil keep it. In most regions the allocation, not the pump, is the binding limit.

Work out where the water actually went

Two dry years is a measurement, not a diagnosis. Ask whether the crop was short of water or short of access to it. A crop that wilts days after rain, on a parcel that got its normal allocation, was not short of supply.

Three failure modes cover most cases: a coarse sandy soil whose large pores drain much of every event below the root zone; a plough pan holding roots above the water beneath it; and low organic matter, which lowers water-holding capacity across the profile.

Separate them with a soil analysis — texture, organic matter, pH, cation-exchange capacity, water-holding capacity — and a spade pit showing where roots stop. If the reserve is decent and roots reach it, the problem is delivery, and the irrigation is the right project.

Why more irrigation is the wrong lever for a storage problem

A soil with a small reserve loses a large share of every event below the root zone, whatever the emitter does. Drip does not change the pore-size distribution of a sand. Smaller, more frequent events help, since each fits the storage that exists, but they cost energy, labour and weekly scheduling. Abstraction is capped, and restrictions arrive in the years the water is needed.

Where delivery really is the constraint — uneven distribution, scheduling on habit, no soil-moisture data — the irrigation upgrade is the answer, and no amendment replaces it.

What actually raises the soil's own reserve

Raising the reserve means changing the soil: more organic matter, more fine mineral surface, more stable aggregates, more pores in the range that holds water at tensions a root can overcome.

Read the last two columns together. A lever that acts in one season and fades in one solves a cash-flow problem, not a soil problem.

LeverWhat it changesTime to effectPersistence
Organic matter, compost, manureRaises retention and structure; slow to buildTwo to ten yearsLost if practice stops
Cover cropsAdd carbon and roots; use intercrop waterOne to three seasonsHolds while rotation holds
Reduced tillageProtects aggregates and fungal networksThree to five yearsUndone by one deep pass
MulchingCuts evaporation; nothing for storageImmediateOne season, then repeat
Clay or bentoniteRaises CEC and retention; tonnages largeFirst seasonPermanent once incorporated
BiocharPorous, persistent; quality and price varyOne to two seasonsLong, but site-dependent
Superabsorbent polymers, hydrogelsFast gain; falls with salinity and cyclingImmediateShort against usual claims

Where a hybrid mineral-biological amendment fits

Hydrobio by KUZOG sits in that table as a storage lever with a biological component. Its clay-based micronised matrix presents about 200 times the specific surface of the unground mineral: small pores holding water by capillarity at tensions the plant can overcome, and a high cation-exchange capacity holding potassium, calcium, magnesium and ammonium against percolation.

The second phase is a living mycorrhizal consortium whose hyphae reach pores narrower than a root hair. The mineral is the scaffold, so the biology establishes where a bare inoculant would not.

On sandy soils under South Europe and MENA conditions, water retention rose by 47% and yield by 18.7% against an untreated control on the same soil type — controlled trials, to be confirmed in independent field trials. One application lasts three to five years, spread with the spreader already in the shed and lightly incorporated at soil preparation.

Where it does not fit, and what it will not do

It does not add water, and it will not compensate for a rainfall deficit on its own. Nor will it fix compaction: a plough pan is a tillage and traffic problem.

It is not a fertiliser and does not replace a nutrition plan. On many parcels a well-run organic-matter and cover-crop programme is the right first move, and cheaper.

It is also not on the shelf today: the patent application is filed with the USPTO — filed, not granted — with a PCT extension underway, EU 2019/1009 homologation in preparation, and broader French commercialisation planned from late 2026, after the deployments now underway.

What to send us for a soil analysis

Composition and dose are set per parcel, so the conversation starts with the parcel. HydrobioFormul, our machine-learning formulation engine, turns what you send into the exact composition, the per-parcel dose and the schedule, on a traced sheet.

  • A recent soil analysis: texture, organic matter, pH, CEC, water-holding capacity — or we support the sampling.
  • The crop and the rotation.
  • The rainfall and irrigation context: allocation, dry-year restrictions, the system in place.
  • The objective: hold yield through a dry summer, cut irrigation hours, revive a failing block.

Questions we are asked

How much yield will I get back?
We publish one figure: 18.7% against an untreated control on sandy soils, in controlled trials still to be confirmed in independent field trials. No recovery of a specific loss can be promised for an unanalysed parcel.
Is the 30% I lost recoverable?
Part of it is a soil problem, part was the weather, and only the analysis separates them. A larger reserve shortens the periods the crop spends under water stress, where most drought loss is made.
Should I upgrade the irrigation or amend the soil first?
Let the analysis decide. If the reserve is decent and roots reach it, the constraint is delivery; if it is small, or roots stop at a compacted layer, more delivery buys more drainage.
Can I not just add compost and cover crops?
Often you should: over a decade it is the more robust lever. But one percent of organic matter takes years and is lost if the practice stops, while a mineral amendment acts in the season it is incorporated.
Does it work on a heavy clay soil?
The measured gains are on sandy soils, where drainage below the root zone is the failure mode. A clay soil failing in drought usually has a structure or compaction problem, answered with tillage and organic matter.
Can I buy it for next season?
Not generally, not yet. First deployments are underway and broader French commercialisation is planned from late 2026, with the patent application filed and EU 2019/1009 homologation in preparation.

Send us the parcel, not the postcode

A soil analysis, the crop and the rainfall context are enough for us to say whether this is a storage problem, a delivery problem or a compaction problem — and whether Hydrobio belongs in the answer. We reply within one business day.

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