A center-pivot irrigation boom sweeping across a green circular field, seen from the air

Saline Ag Supercharge

The root zone runs short of air before it runs short of water.

Put oxygen into the wetted bulb and the crop answers: cotton lint up 26 percent on a Vertosol under subsurface drip. NanoponiX measures the number on your own block first, then holds a target dissolved oxygen at the emitter through the irrigation events on that source, on a subscription written to what the block showed.

1,381 Mha Salt-affected soils worldwide, 10.7% of global land area; roughly a tenth of irrigated cropland is affected FAO, Global status of salt-affected soils
+26% Cotton lint yield under oxygated subsurface drip against non-aerated drip, on a Vertosol Bhattarai & Midmore, Crop & Pasture Science
+11.15% Water-use efficiency across 2,398 data pairs from 35 studies of micro-nanobubble irrigation Plant and Soil, 2026

The agronomy

Irrigation is discussed as a water problem. Sometimes it is a gas problem.

Soil is roughly half solid and half pore space, shared between water and air. Every irrigation event pushes air out. On a light, well-structured soil it comes back quickly. On a heavy clay, a sodic profile or a compacted headland it comes back slowly, and meanwhile the roots and their microbial community keep respiring.

Subsurface drip sharpens this. Its advantage is holding the wetted bulb near field capacity for longer, which is what a breathing root does not want. The better your irrigation efficiency, the harder you can push the root zone toward hypoxia.

Salinity stacks on top. A root spending energy on osmotic adjustment has less left for anything else, and a hypoxic root excludes sodium less well than an aerobic one. Two stresses, each worsening the other.

Oxygation puts air or oxygen into the irrigation stream so the bulb is not anoxic. The idea is decades old. What has changed is how much oxygen stays in the water on the way to the emitter.

What the trials measured

Published results, from other growers' fields.

Other crops, other soils.

24.6 t/ha Watermelon fruit yield under oxygation, up from 14.5 t/ha on the control; heavy clay, semi-arid tropics, soluble solids up 19% Bhattarai, Dhungel & Midmore, 2010
+29–41% Maize yield under micro-nanobubble drip with phosphorus, with agronomic phosphorus-use efficiency up to 134.91% higher at reduced P rates Bian et al., Plants, 2024
+13.55% Mean crop yield response across the same 35-study micro-nanobubble meta-analysis; root dry weight up about 27% Plant and Soil, 2026

Response varies

One trial, one soil, a sevenfold gap between two crops.

In that 2010 cucurbit trial, on the same heavy clay, in the same season, under the same treatment, watermelon fruit yield rose from 14.5 to 24.6 tonnes per hectare. Pumpkin rose from 26.3 to 28.9.

One of those is about seventy percent. The other is about ten.

Crop, soil, irrigation method and the starting oxygen deficit all move the response.

So a program starts with a paired block trial: treated and control on the same soil unit, target oxygen at the emitter and sampling interval written down before the first irrigation, yield read by a laboratory both sides can name. A local agricultural research station or university irrigation department holds the water-side logs as an independent witness.

Dense rows of spinach growing under glass in a controlled-environment greenhouse
Controlled environments narrow the variables: the fastest place to learn whether a response exists.

The sharpest case

Growers already irrigating with water that is hurting them.

FAO's global assessment puts salt-affected soils at about 1,381 million hectares, some 10.7 percent of the world's land, with roughly a tenth of both irrigated and rainfed cropland affected. Ten countries hold seventy percent of it. In much of the Gulf, North Africa and the drier parts of Central and South Asia, the water available for irrigation is brackish. The choice is brackish water or no crop.

Saline Ag Supercharge is built for those growers. Salinity and root-zone hypoxia are separate stresses that amplify one another, and oxygation acts on one of the two directly.

It does not act on the other. Salt applied is salt delivered, and nothing put through an emitter changes the ionic load of the water.

The stress arrives every time the valve opens, so the service runs standing. A root zone held aerobic from the first irrigation never spends a crop catching up, which keeps the price down; a block already going backward would be priced as a rescue.

Oxygation on brackish and saline ground

A white salt crust stretching to distant hills across a dry flat
Brackish irrigation water accumulates salt in the profile. Drainage and leaching stay the grower's problem.

Scope

Where the treatment stage stops and the agronomy starts.

What a program answers for on your ground, and what stays with the farm.

  • It does not desalinate. Water leaves the emitter at the electrical conductivity it went in with.
  • It does not substitute for leaching or drainage. If the profile has nowhere to send accumulated salt, no treatment through the irrigation line gives it one.
  • It comes with no yield guarantee, and none will be written. The published response spans roughly ten to seventy percent between two crops in a single trial, too wide to underwrite.
  • It is not a reason to re-lay your system. The stage sits in-line ahead of your existing filtration and distribution, and your laterals and emitters stay where they are.
  • It does not settle agriculture's nutrient export problem on its own. USGS basin modeling of the Mississippi and Atchafalaya puts farming as the largest source of the nitrogen and phosphorus reaching the Gulf, and cutting that at source is a twenty-year job. Phosphorus doing more work per kilogram helps. So does an oxidation and aeration firewall on a runoff hotspot, taking the load where it leaves the ground. Dr Peter Moeller of NOAA observed an effect on nitrogen and phosphorus in this chemistry; it is still under study, NOAA endorses nothing, and no number is published. Fertilizer feeds people, and it does not have to lose for water to win.

The other half of the job

Storage reservoirs, algae and blocked emitters.

Most irrigation schemes store water first. In a hot climate, it grows algae.

Algal load in a farm reservoir reaches the filter station, shortens backwash intervals, slips past screens as fine organic matter and ends up as biofilm inside laterals and emitters. Subsurface drip on surface-stored water fights this part of every year.

NCCOS, NOAA's coastal science arm, validated an ozone nanobubble aeration system on an eight-acre freshwater pond in Florida in 2018 and reported algae eliminated within 48 hours, oxygen restored, and no apparent harm to the life in the pond. A farm storage reservoir is far more like that pond than a field is.

NABAS, the rig in that pond, was another company's.

An abandoned wooden boat sitting in a lake whose surface is thickly covered in green algae
Stored water answers fastest, which is why storage usually goes first on a mixed site.
48 hours To complete elimination of algae on an eight-acre freshwater pond, with reoxygenation and no apparent harm to aquatic life NOAA NCCOS, September 2018
1.5× Oxygen transfer efficiency for nanobubble aeration against coarse bubbles, from the abstract of a laboratory study; comparable work reports other figures Science of the Total Environment

Both trials and the papers behind them.

Aerial view of circular irrigated fields beside a winding river

Immediate, Significant, Scaled

Bring us a block and a water analysis.

Crop, soil type, irrigation method, water quality, and what your yield has been doing. Alarivean replies with whether a response is plausible on that ground, and how cheaply you could find out.