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HCT UNIVERSITY · IRRIGATION WATER QUALITY

Your water is more than H₂O. Here is what it carries, and what to do about it.

Irrigation water carries minerals, salts, bicarbonates, sodium, chloride, and biology. With every cycle, each one either helps the site or adds another layer of stress. This page explains what is in the water, how it becomes scale, sealed soil, and tied-up nutrition, and how WaterSOLV™ conditions the water at the source so irrigation works for the crop or turf instead of against it.

For growers, turf managers, and golf course superintendents · Agriculture, turf, and landscape irrigation · Testing before treatment

WHAT WATER QUALITY MEANS

Water quality is how your water behaves once it enters the soil-water-plant system.

It is not a pH number or a lab sheet. It is whether dissolved nutrients stay soluble, how salts behave as the water evaporates, whether oxygen stays available in the profile, and whether each irrigation supports or restricts infiltration and plant response. Water can test acceptable and still behave badly in the field, which is why interpretation matters as much as the numbers.

 

In the field it shows up as ponding, sealing, and runoff; white crust, scale, and residue; uneven response after irrigation or fertility; and acid use that keeps climbing.

Watch: what HCT sees in problem irrigation water and how WaterSOLV™ changes it.

WHAT IS IN THE WATER

Four things in irrigation water that work against the site.

They rarely act alone: bicarbonate, sodium, chloride, and biology feed each other, so correcting a single number rarely corrects the field. Each has its own HCT University page.

01

 

Bicarbonates and hardness

 

Calcium and magnesium bond with bicarbonate as water evaporates, forming scale on emitters and cemented soil, and locking up nutrients.

 

Bicarbonates →

02

 

Sodium and chloride

 

Sodium tightens the profile and cuts infiltration; chloride salts crust and stress the plant. Both stay concentrated where roots feed.

 

Sodium and chloride →

03

 

Bacteria and biofilm

 

Slime narrows flow paths, holds moisture in the wrong zone, and pushes the root zone toward anaerobic, black-layer conditions.

 

Biology →

04

 

Lost oxygen

 

Once the profile stays tight or saturated, oxygen falls and biology turns septic: odor, slow recovery, uneven response.

 

Infiltration →

WHY QUICK FIXES DON’T HOLD

Lower pH is not the same as fixing the water.

The usual answers treat a reading or a symptom while the minerals, salts, and biology keep arriving with every cycle.

SULFURIC ACID

 

Drops the pH, leaves the chemistry

 

Lines look clean for a while, then the minerals reform after evaporation into deposits that further acid does not readily redissolve. Added sulfate feeds black-layer bacteria and the acid corrodes pumps, valves, and fittings.

 

Sulfuric acid vs. WaterSOLV →

GYPSUM AND FLUSHING

 

Only work if water can already move

 

Calcium additions and heavy leaching depend on a profile that can still take water. On a sealed, sodium-tightened profile the flush stays at the surface and the salts stay in the root zone.

 

Sodium and chloride →

CHLORINE

 

Kills what floats, misses what sticks

 

Chlorine disinfects free-floating bacteria but does not readily penetrate the biofilm where colonies live. Survivors recolonize faster, and it corrodes the equipment it passes through.

 

Chlorine vs. WaterSOLV BC →

HOW WATERSOLV CONDITIONS THE WATER

Treat the water at the source, and every irrigation cycle starts working for you.

WaterSOLV™ is injected at the pump station during normal irrigation, through the same point an acid program uses. Instead of chasing a pH reading, it changes what the minerals and the biology do after the water leaves the emitter.

01

 

Keeps scale-forming minerals soluble

 

WATERSOLV™ CURATIVE

 

A buffered acid-based sequestering chemistry. It breaks apart the calcium–magnesium bicarbonate crystal structure and satisfies the charge so calcium and magnesium stay soluble and plant-available. Treated minerals dry to a fine powder instead of hard scale and go back into solution when water returns.

02

 

Takes the pressure off sodium and chloride

 

CONDITIONED WATER, DEEPER WETTING

 

Sodium and chloride are addressed in the water before plant uptake, and as the profile opens up, water moves deeper and more evenly. Salts stop sitting in the active root zone and leaching works again, because flushing only works when the profile can take water.

03

 

Clears biofilm and restores oxygen

 

WATERSOLV™ BC

 

Hydrogen peroxide with acetic acid. It penetrates and breaks down biofilm, reduces anaerobic bacterial activity, and delivers oxygen to the root zone. It biodegrades to oxygen and water, adds no nitrogen or sulfur, is corrosion-inhibited (the SDS classifies it as corrosive to skin and eyes), and is NSF/ANSI/CAN 60 listed for well cleaning.

PRODUCT VOLUME

 

Up to 90% less product than acid programs

 

Rates are set from analysis, but WaterSOLV™ runs at a fraction of the volume of continuous acid injection.

WHAT IT DOES NOT ADD

 

No sulfuric acid, no urea, no added nutrients

 

Nothing to feed black layer or push soft growth. Corrosion-inhibited; handle per the SDS.

HOW IT IS SIZED

 

The water sets the rate

 

One almond block at 372 mg/l bicarbonate called for 4.21 ppm Curative; a lighter 100 mg/l source next door called for 1.01 ppm.

WHAT THE CASE STUDIES SHOW

Difficult water, measured before and after.

EAGLES NEST COUNTRY CLUB · TURF

 

Bad water made valuable

 

Free but difficult water at 7.5 ppm Curative and 0.25 ppm BC. In six months soil sodium fell and CEC rose.

 

572 → 402

soil sodium, ppm · CEC 42.8 → 62

 

Turf case studies →

WILDHORSE GOLF CLUB · TEXAS

 

Drain water cleared in 90 days

 

Eight years of French drains had not fixed the squish; treating the water did. Lowest drain-water EC of the superintendent’s tenure.

 

EC 0.9

drain water · pH 7.8

 

Turf case studies →

BAPU FARMS · ALMONDS AND PISTACHIOS

 

Hard, salty water; more nuts per acre

 

Source water at 372 mg/l bicarbonate, 470 ppm hardness, 122 mg/l sodium. Treated blocks out-yielded untreated through a no-rain season.

 

+14% · +12%

almonds · pistachios, lbs/acre

 

Agriculture case studies →

VALIDATE, THEN TREAT

Start with the water. The numbers set the program.

An irrigation water analysis (bicarbonate, hardness, sodium, chloride) sets the Curative rate. A bacteria count decides whether BC belongs in the program. A soil analysis covers the profile where it is part of the problem. Send HCT your water and the symptoms you are seeing, and you will get a read on what is driving them and whether a WaterSOLV™ program fits.

KEEP LEARNING

HCT, LLC · HCT University · Irrigation Water Quality · Scottsdale, Arizona

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