Chalybeate Spring, Mittagong
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Chalybeate Spring, Mittagong
The Chalybeate Spring at Mittagong, New South Wales was a perennial, carbonated, chalybeate (iron-rich) mineral spring Successive chalybeate springs at Mittagong had, over many thousands of years, created a deposit of iron ore that was mined by the Fitzroy Iron Works, which was closely associated with the early development of the town of Mittagong, in the Southern Highlands of New South Wales, Australia. The spring was for many years a tourist attraction, mainly during the second half of the 19th century and first few decades of the 20th century. Early history Aboriginal context The traditional owners of the country around Mittagong are the Gandangara people. It is not known if they used the spring as a water source but this small spring, given its strong-tasting water and earthy odour, would be an unlikely water source, with plentiful freshwater nearby. It is almost certain that the limonite in the area surrounding the spring would have been used as ochre pigment. Disco ...
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Chalybeate
Chalybeate () waters, also known as ferruginous waters, are mineral spring waters containing salts of iron. Name The word ''chalybeate'' is derived from the Latin word for steel, , which follows from the Greek word . is the singular form of or Chalybes, who were a people living on Mount Ida in north Asia Minor and who were expert in iron working. ''Ferruginous'' () comes from the Latin word 'of a rusty colour', from 'iron rust', from 'iron'. History Early in the 17th century, chalybeate water was said to have health-giving properties and many people once promoted its qualities. Dudley North, 3rd Baron North, discovered the chalybeate spring at Tunbridge Wells in 1606. His eldest son's physician said the waters contained "vitriol" and the waters of Tunbridge Wells could cure: the colic, the melancholy, and the vapours; it made the lean fat, the fat lean; it killed flat worms in the belly, loosened the clammy humours of the body, and dried the over-moist brain. He also ...
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Hill Top, New South Wales
Hill Top is a Northern Village of the Southern Highlands of New South Wales, Australia, in Wingecarribee Shire. Previous names of the village include ''Hilltop'' and ''Jellore''. It is a 17 km drive to Mittagong and around 10 km drive to the Hume Highway via Colo Vale. It is roughly 6–8 km to Yerrinbool as the crow flies. History It was formerly on the Main Southern Railway, until that line was deviated in 1919 to a less steep alignment with easier grades. The original line became the Picton Loop line, which closed in 1978. The remains of Hill Top station platform can still be seen. Facilities Hill Top has commercial facilities such as a pizzeria, bakery, chemist, general store, liquor store, real estate agent, and GP's surgery. Community facilities include a post office, tennis courts, sporting fields, day-care centre, primary school, fire station, church and community hall. It is home to the Southern Highlands Rifle Club's shooting range. In 2007, con ...
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Fitzroy Iron Ore Deposit Mittagong Map (Jaquet, 1901, P51)
Fitzroy or FitzRoy may refer to: People As a given name *Several members of the Somerset family (Dukes of Beaufort) have this as a middle-name: **FitzRoy Somerset, 1st Baron Raglan (1788–1855) ** Henry Charles FitzRoy Somerset, 8th Duke of Beaufort (1824–1899) ** Henry Adelbert Wellington FitzRoy Somerset, 9th Duke of Beaufort (1847–1924) ** Henry Hugh Arthur FitzRoy Somerset, 10th Duke of Beaufort (1900–1984) ** Henry FitzRoy Somerset, 12th Duke of Beaufort (born 1952), called Bunter Worcester *Fitzroy Alexander (1926–1988), better known as Lord Melody, a calypsonian from Trinidad * Sir Fitzroy Maclean (1911-1996), Scottish soldier, writer and politician As a surname * Fitzroy (surname), i.e. not the form FitzRoy Descendants of Charles II and Barbara Palmer * Anne Lennard, Countess of Sussex or Lady Anne Fitzroy (1661–1722), daughter of King Charles II of England and Barbara Palmer, 1st Duchess of Cleveland * Charles FitzRoy, 2nd Duke of Cleveland (1662–1730), son ...
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Aqueous Solution
An aqueous solution is a solution in which the solvent is water. It is mostly shown in chemical equations by appending (aq) to the relevant chemical formula. For example, a solution of table salt, or sodium chloride (NaCl), in water would be represented as . The word ''aqueous'' (which comes from ''aqua'') means pertaining to, related to, similar to, or dissolved in, water. As water is an excellent solvent and is also naturally abundant, it is a ubiquitous solvent in chemistry. Since water is frequently used as the solvent in experiments, the word solution refers to an aqueous solution, unless the solvent is specified. A ''non-aqueous solution'' is a solution in which the solvent is a liquid, but is not water. (See also Solvent and Inorganic nonaqueous solvent.) Characteristics Substances that are ''hydrophobic'' ('water-fearing') do not dissolve well in water, whereas those that are ''hydrophilic'' ('water-friendly') do. An example of a hydrophilic substance is sodium chlo ...
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Magnesium Chloride
Magnesium chloride is the family of inorganic compounds with the formula , where x can range from 0 to 12. These salts are colorless or white solids that are highly soluble in water. These compounds and their solutions, both of which occur in nature, have a variety of practical uses. Anhydrous magnesium chloride is the principal precursor to magnesium metal, which is produced on a large scale. Hydrated magnesium chloride is the form most readily available. Production Magnesium chloride can be extracted from brine or sea water. In North America, it is produced primarily from Great Salt Lake brine. In the Jordan Valley, it is obtained from the Dead Sea. The mineral bischofite () is extracted (by solution mining) out of ancient seabeds, for example, the Zechstein seabed in northwest Europe. Some deposits result from high content of magnesium chloride in the primordial ocean. Some magnesium chloride is made from evaporation of seawater. In the Dow process, magnesium chloride is regen ...
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Potassium Chloride
Potassium chloride (KCl, or potassium salt) is a metal halide salt composed of potassium and chlorine. It is odorless and has a white or colorless vitreous crystal appearance. The solid dissolves readily in water, and its solutions have a salt-like taste. Potassium chloride can be obtained from ancient dried lake deposits. KCl is used as a fertilizer, in medicine, in scientific applications, domestic water softeners (as a substitute for sodium chloride salt), and in food processing, where it may be known as E number additive E508. It occurs naturally as the mineral sylvite, and in combination with sodium chloride as sylvinite. Uses Fertilizer The majority of the potassium chloride produced is used for making fertilizer, called potash, since the growth of many plants is limited by potassium availability. Potassium chloride sold as fertilizer is known as muriate of potash (MOP). The vast majority of potash fertilizer worldwide is sold as MOP. Medical use Potassium is vital ...
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Sodium Chloride
Sodium chloride , commonly known as salt (although sea salt also contains other chemical salts), is an ionic compound with the chemical formula NaCl, representing a 1:1 ratio of sodium and chloride ions. With molar masses of 22.99 and 35.45 g/mol respectively, 100 g of NaCl contains 39.34 g Na and 60.66 g Cl. Sodium chloride is the salt most responsible for the salinity of seawater and of the extracellular fluid of many multicellular organisms. In its edible form, salt (also known as ''table salt'') is commonly used as a condiment and food preservative. Large quantities of sodium chloride are used in many industrial processes, and it is a major source of sodium and chlorine compounds used as feedstocks for further chemical syntheses. Another major application of sodium chloride is de-icing of roadways in sub-freezing weather. Uses In addition to the familiar domestic uses of salt, more dominant applications of the approximately 250 million tonnes per year production (2008 ...
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Calcium Bicarbonate
Calcium bicarbonate, also called calcium hydrogencarbonate, has the chemical formula Ca(HCO3)2. The term does not refer to a known solid compound; it exists only in aqueous solution containing calcium (Ca2+), bicarbonate (), and carbonate () ions, together with dissolved carbon dioxide (CO2). The relative concentrations of these carbon-containing species depend on the pH; bicarbonate predominates within the range 6.36–10.25 in fresh water. All waters in contact with the atmosphere absorb carbon dioxide, and as these waters come into contact with rocks and sediments they acquire metal ions, most commonly calcium and magnesium, so most natural waters that come from streams, lakes, and especially wells, can be regarded as dilute solutions of these bicarbonates. These hard waters tend to form carbonate scale in pipes and boilers and they react with soaps to form an undesirable scum. Attempts to prepare compounds such as solid calcium bicarbonate by evaporating its solution to dr ...
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Magnesium Bicarbonate
Magnesium bicarbonate or magnesium hydrogencarbonate, Mg( H CO3)2, is the bicarbonate salt of magnesium. It can be formed through the reaction of dilute solutions of carbonic acid (such as seltzer water) and magnesium hydroxide (milk of magnesia). It can be prepared through the synthesis of magnesium acetate and sodium bicarbonate: :: Magnesium bicarbonate exists only in aqueous solution. Magnesium does not form solid bicarbonate as does lithium. To produce it, a suspension of magnesium hydroxide is treated with pressurized carbon dioxide, producing a solution of magnesium bicarbonate: ::Mg(OH)2 + 2 CO2 → Mg(HCO3)2 Drying the resulting solution causes the magnesium bicarbonate to decompose Decomposition or rot is the process by which dead organic substances are broken down into simpler organic or inorganic matter such as carbon dioxide, water, simple sugars and mineral salts. The process is a part of the nutrient cycle and is ..., yielding magnesium carbonate, ca ...
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Parts Per Million
In science and engineering, the parts-per notation is a set of pseudo-units to describe small values of miscellaneous dimensionless quantities, e.g. mole fraction or mass fraction. Since these fractions are quantity-per-quantity measures, they are pure numbers with no associated units of measurement. Commonly used are parts-per-million (ppm, ), parts-per-billion (ppb, ), parts-per-trillion (ppt, ) and parts-per-quadrillion (ppq, ). This notation is not part of the International System of Units (SI) system and its meaning is ambiguous. Overview Parts-per notation is often used describing dilute solutions in chemistry, for instance, the relative abundance of dissolved minerals or pollutants in water. The quantity "1 ppm" can be used for a mass fraction if a water-borne pollutant is present at one-millionth of a gram per gram of sample solution. When working with aqueous solutions, it is common to assume that the density of water is 1.00 g/mL. Therefore, it is common to equat ...
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Spring (hydrology)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels through ...
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Carbonated Water
Carbonated water (also known as soda water, sparkling water, fizzy water, club soda, water with gas, in many places as mineral water, or especially in the United States as seltzer or seltzer water) is water containing dissolved carbon dioxide gas, either artificially injected under pressure or occurring due to natural geological processes. Carbonation causes small bubbles to form, giving the water an effervescent quality. Common forms include sparkling natural mineral water, club soda, and commercially-produced sparkling water. Club soda and sparkling mineral water and some other sparkling waters contain added or dissolved minerals such as potassium bicarbonate, sodium bicarbonate, sodium citrate, or potassium sulfate. These occur naturally in some mineral waters but are also commonly added artificially to manufactured waters to mimic a natural flavor profile and offset the acidity of introducing carbon dioxide gas. Various carbonated waters are sold in bottles and cans, with some ...
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