Seawater is a complex solution dominated by dissolved salts, gases, nutrients, trace metals, and organic compounds. Despite geographical variation in salinity, the relative proportions of major ions remain remarkably constant worldwide, a concept known as the Principle of Constant Proportions. The majority of seawater salinity is contributed by chloride, sodium, sulfate, magnesium, calcium, and potassium.
Regional differences mainly occur in semi-enclosed basins and high-evaporation zones (e.g., Arabian Gulf, Red Sea), while open-ocean regions across North America, Europe, and South America exhibit more stable concentrations.
Major ion composition of seawater (mg/L):
Representative concentration ranges (mg/L) by global region
Values reflect typical seawater at ~35 PSU; higher-evaporation regions show slightly elevated ion levels.
| Major Ion | West Asia & Middle East | North America | North Africa | Europe | South & Central America | Other (Global Open Ocean) |
|---|---|---|---|---|---|---|
| Chloride (Cl⁻) | 19,000 – 21,000 | 18,500 – 19,500 | 18,800 – 20,000 | 18,600 – 19,600 | 18,500 – 19,400 | ~19,000 |
| Sodium (Na⁺) | 10,500 – 11,600 | 10,200 – 10,800 | 10,400 – 11,200 | 10,300 – 10,900 | 10,200 – 10,800 | ~10,500 |
| Sulfate (SO₄²⁻) | 2,700 – 3,000 | 2,600 – 2,800 | 2,650 – 2,900 | 2,600 – 2,850 | 2,600 – 2,800 | ~2,700 |
| Magnesium (Mg²⁺) | 1,300 – 1,450 | 1,250 – 1,350 | 1,280 – 1,400 | 1,260 – 1,360 | 1,250 – 1,340 | ~1,300 |
| Calcium (Ca²⁺) | 380 – 450 | 380 – 420 | 380 – 430 | 380 – 420 | 380 – 410 | ~400 |
| Potassium (K⁺) | 360 – 420 | 360 – 400 | 360 – 410 | 360 – 400 | 360 – 390 | ~380 |
| Bicarbonate (HCO₃⁻) | 120 – 160 | 110 – 140 | 115 – 145 | 110 – 140 | 110 – 135 | ~130 |
| Bromide (Br⁻) | 60 – 75 | 60 – 70 | 60 – 72 | 60 – 70 | 60 – 68 | ~65 |
| Strontium (Sr²⁺) | 7 – 10 | 7 – 9 | 7 – 9 | 7 – 9 | 7 – 9 | ~8 |
| Boron (as B) | 4 – 6 | 4 – 5 | 4 – 5 | 4 – 5 | 4 – 5 | ~4.5 |
Seawater Desalination Systems
Water Softner
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West Asia & Middle East values trend slightly higher due to higher evaporation basins (Arabian Gulf, Red Sea).
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North America, Europe, and South/Central America reflect stable open-ocean chemistry.
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Minor variation occurs due to river discharge, temperature, seasonal mixing, and local salinity.
Source: Water Conditioning & Purification Magazine, January 2005
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Frequently Asked Questions
What are the primary dissolved components and average salinity of seawater?
The average global ocean salinity is 35 parts per thousand (PSU), equivalent to 35,000 mg/L TDS. Seawater is predominantly composed of six major ions: chloride (~55%), sodium (~31%), sulfate (~8%), magnesium (~3.7%), calcium, and potassium, which together constitute over 99% of its dissolved salts.
How does seawater’s chemical composition impact the design of desalination systems?
Understanding seawater’s precise chemical composition is crucial for designing effective desalination systems. Ionic concentrations directly influence membrane selection, required operating pressure (typically 55–80 bar for SWRO), pre-treatment chemistry, and energy consumption, ensuring optimal system performance and longevity. AMPAC USA engineers leverage this knowledge for robust system design.
What is the Principle of Constant Proportions in oceanography?
The Principle of Constant Proportions, also known as the Marcet Principle, states that while the total salinity of seawater varies regionally, the relative ratios of its major dissolved ions remain remarkably constant worldwide. This principle allows engineers to accurately estimate the full ion profile and design reverse osmosis systems from a single salinity measurement, simplifying complex calculations.
What is the typical osmotic pressure of seawater and the operating pressure for SWRO systems?
At an average salinity of 35 PSU, seawater exhibits an osmotic pressure of approximately 27 bar (390 PSI). To effectively overcome this natural osmotic pressure and produce freshwater, Seawater Reverse Osmosis (SWRO) systems typically operate at high pressures ranging from 55–80 bar (800–1,160 PSI) at standard recovery rates.
Why is detailed knowledge of seawater composition essential for AMPAC USA’s desalination projects?
Detailed knowledge of seawater composition is essential for AMPAC USA because it underpins the design of highly efficient and reliable commercial and industrial desalination systems. Our 30+ years of field experience, from offshore oil rigs to military bases, demonstrates how precise understanding of ionic concentrations dictates optimal membrane selection, pre-treatment strategies, and energy-efficient operation, ensuring our systems perform reliably in diverse global environments.
AMPAC USA engineers custom water purification systems for commercial, industrial, and emergency applications — from 500 GPD to multi-million GPD. Trusted by municipalities, military, and industry worldwide.

