SALT, SEA

or CULINARY; Chloride of sodium ; muriate of soda . ( Hydro chlorate de soude , Fr.; Chlornatrium , Germ.) Sea salt, or rock salt, in a state of purity, consists of 60 of chlorine + 40 of sodium, in 100 parts. This important species of the saline cla po e es, even in ma , a crystalline structure, derived from the cube, which is its primitive form. It has generally a foliated texture, and a distinct cleavage; but it has also sometimes a fibrous structure. The ma ive salt has a vitreous lustre. It is not so brittle as nitre; it is nearly as hard as alum, a little harder than gypsum, and softer than calcareous spar. Its specific gravity varies from 2·0 to 2·25. When pure, it is colourle , translucent, or transparent. On exposure to heat, it commonly decrepitates; but some kinds of rock salt enter quietly into fusion at an elevated temperature, a circumstance which has been ascribed to their having been originally subjected to the action of fire. According to M. Gay Lu ac, 100 parts of water di olve — | 35·81 | parts of the salt, at temperature | 57·0° | Fahr. | | 35·88 | — | 62·5° | | | 37·14 | — | 140·0° | | | 40·38 | — | 229·5° | | Native chloride of sodium, whether obtained from the waters of the ocean, from saline lakes, from salt springs, or mineral ma es, is never perfectly pure. The foreign matters present in it vary with its different origins and qualities. These are, the sulphates of lime, magnesia, soda, muriates of magnesia and potash, bitumen, oxide of iron, clay in a state of diffusion, . Muriate of potash has been detected, in the waters of the ocean, in the sal-gem of Berchtesgaden in Bavaria, of Hallein in the territory of Salzbourg, and in the salt springs of Rosenheim. The more heterogeneous the salt, the more soluble is it, by the reciprocal affinity of its different saline constituents; and thus a delicate hydrometer, plunged in saturated brine, may serve to show approximately the quality of the salt. I find that the specific gravity of a saturated solution of large-grained cubical salt, is 1·1962 at 60° F. 100 parts of this brine contain 25 1 ⁄ 2 of salt, (100 w. + 34·2 s.) From mutual penetration, 100 volumes of the aqueous and saline constituents form rather le than 96 of the solution. Among the varieties in the form of this salt, the octahedral, the cubo-octahedral, and the dodecahedral, have been mentioned; but there is another, called the funnel or hopper-shaped, which is very common. It is a hollow rectangular pyramid, which forms at the surface of the saline solution in the course of its evaporation, commencing with a small floating cube, upon which lines of other little cubes attach themselves to the edges of the upper face; whereby they form and enlarge the sides of a hollow pyramid, whose apex, the single cubic crystal, is downward. This sinks by degrees as the aggregation goes on above, till a pyramidal boat of considerable size is constructed. A Table of the results of the Analyses of several varieties of Culinary Salt . | Origin of the Salt. | Chloride of Sodium. | Muriate of Mag- nesia. | Muriate of Lime. | Sulphate of Soda. | Sulphate of Mag- nesia. | Sulphate of Lime. | Clay and other insoluble bodies. | Oxide of Iron. | | Sal-gem of Vic | - | | white | 99 | ·30 | — | — | — | — | 0 | ·005 | 0 | ·020 | | | red | 99 | ·80 | — | — | — | — | — | 0 | ·002 | | | —— Cheshire, crushed | 98 | ·33 | 0 | ·02 | — | — | — | 0 | ·65 | — | 0 | ·002 | | Salt from Salt Springs: | | | | | | | | | | Schönbeck, Westphalia | 93 | ·90 | 0 | ·30 | — | 1 | ·00 | — | 0 | ·80 | | | | Moutiers | - | | des cordes | 97 | ·17 | 0 | ·25 | — | 2 | ·00 | 0 | ·58 | | | | | boilers | 93 | ·59 | 0 | ·61 | — | 5 | ·55 | 0 | ·25 | | | | | Château Salins | 97 | ·82 | 2 | ·12 | | | | | | | | White of Sulz | 96 | ·88 | 3 | ·12 | | | | | | | | Lud wig shall, middle grained | 99 | ·45 | — | — | 0 | ·05 | — | 0 | ·28 | | | | Kœnigsborn, Westphalia | 95 | ·90 | — | 0 | ·27 | — | — | 1 | ·10 | | | | Sea salt, half white | 97 | ·20 | 0 | ·004 | — | — | 0 | ·050 | 0 | ·120 | 0 | ·070 | | | ——, of Saint Malo | 96 | · | 0 | ·30 | — | — | 0 | ·45 | 2 | ·35 | | | | Common Scottish salt | 93 | ·55 | 2 | ·80 | — | — | 1 | ·75 | 1 | ·50 | | | | Lymington, common | 93 | ·7 | 1 | ·1 | — | — | 3 | ·50 | 1 | ·50 | 2 | ·00 | | | ——, cat | 98 | ·8 | 0 | ·5 | — | — | 0 | ·5 | 0 | ·1 | | | | Cheshire, stoved | 98 | ·25 | 0 | ·075 | 0 | ·025 | — | — | 1 | ·55 | | | The geological position of rock salt is between the coal formation and the lias. The great rock-salt formation of England occurs within the red marl , or new red sandstone, the bunter-sand stein of the Germans, so called, because its colours vary from red to salmon and chocolate. This mineral stratum frequently presents streaks of light blue, verdigris, buff, or cream colour; and is chiefly remarkable for containing considerable ma es or beds of gypsum. At North wich, in the vale of the Weaver, the rock salt consists of two beds, together not le than 60 feet thick, which are supposed to constitute large insulated ma es, about a mile and a half long, and nearly 1300 yards broad. There are other deposits of rock salt in the same valley, but of inferior importance. The uppermost bed occurs at 75 feet beneath the surface, and is covered with many layers of indurated red, blue, and brown clay, interstratified more or le with sulphate of lime, and interspersed with argillaceous marl. The second bed of rock salt lies 31 1 ⁄ 2 feet below the first, being separated from it by layers of indurated clay, with veins of rock salt running through them. The lowest bed of salt was excavated to a depth of 110 feet, several years ago. The beds or ma es of rock salt are occasionally so thick, that they have not been yet bored through, though mined for many centuries. This is the case with the immense ma of Wieliczka, and the lower bed at North wich. But in ordinary cases, this thickne varies from an inch or two to 12 or 15 yards. When the strata are thin, they are usually numerous; but the beds, layers, or ma es never exhibit throughout a great extent any more than an illusory appearance of parallelism; for when they are explored at several points, enlargements are observed, and such diminutions as cause the salt to disappear sometimes altogether. This mineral is not deposited, therefore, in a geological stratum, but rather in lenticular ma es, of very variable extent and thickne , placed alongside of each other at unequal distances, and interposed between the courses of the other formations. Sometimes the rock salt is di eminated in small ma es or little veins among the calcareous and argillaceous marls which accompany or overlie the greater deposits. Bitumen, in small particles, hardly visible, but distinguishable by the smell, occurs in all the minerals of the saliferous system. It has been remarked, that the plants which grow generally on the sea shores, such as the Triglochinum maritimum , the Salicornia , the Salsola kali , the Aster trifolium , or farewell to summer, the Glaux maritima , ., occur also in the neighbourhood of salt mines and salt springs, even of those which are most deeply buried beneath the surface. The interior of rock-salt mines, after digging through the strata of clay marl, . is extremely dry; so that the dust produced in the workings becomes an annoyance to the miners, though in other respects the excavations are not at all insalubrious. Salt springs occur nearly in the same circumstances, and in the same geological formation as the salt rock. It has been noticed that salt springs i ue, in general, from the upper portion of the saliferous strata, principally from the saline clay marls. Cases however occur, where the salt springs are not accompanied by rock salt, and where the whole saline matter is derived from the marls themselves, which thus constitute the only saliferous beds. It has been imagined that there are two other periods of geological formation of this substance; one much more antient, belonging to the transition series of rocks; the other relatively modern, among secondary strata. To the former has been referred the salt formation of Bex, that of Car donne, . But M. Brongniart a igns valid reasons for rejecting this supposition. M. Beudant, indeed, refers to the secondary strata above the chalk, the rock-salt formation of Wieliczka, and of the base of the Car path i ans; placing these among the plastic clay and lignites. The mines of rock salt do not appear to po e any determinate elevation upon the surface of the earth. Immense ma es of it are met with at very great depths below the level of the sea, (the mine of Wieliczka is excavated 860 feet beneath the soil,) and others exist at a considerable altitude, as that of Hallein near Salzbourg, which is 3300 feet above the level of the sea, and the saline rock of Arbonne in Savoy, which is nearly 4000 feet higher, situated at the great elevation of 7200 feet above the level of the sea, and consequently in the region of perpetual snow. The rock is a ma of saccharoid and anhydrous gypsum, imbued with common salt, which is extracted by lixiviation; after which the gypsum remains porous and light. The inland seas, salt lakes, and salt marshes, have their several localities obviously independent of peculiar geological formations. The ocean is, however, the most magnificent mine of salt, since this chloride constitutes about one-thirtieth part of its weight; being pretty evenly diffused throughout its waters, when no local cause disturbs the equilibrium. The largest proportion of salt held in solution in the open sea, is 38 parts in 1000, and the smallest 32. In a specimen taken by Mr. Wilkinson, out of the Red Sea, at Berenice, I found 43 parts of salt in 1000. The specific gravity of the water was 1·035. Were it requisite to extract the chloride of sodium from sea-water by fuel alone, many countries, even maritime, would find the proce too costly. The salt is therefore obtained from it in two different manners; 1. by natural evaporation alone; 2. by natural and artificial evaporation combined. The first method is employed in warm regions, under the form of saline tanks, or brine reservoirs, called also brine-pits. These are large shallow basins, the bottom of which is very smooth, and formed of clay. They are excavated along the sea-shore, and consist of — 1st. A large reservoir, deeper than the proper brine-pits, which is dug between them and the sea. This reservoir communicates with the sea by means of a channel provided with a sluice. On the sea-shore, these reservoirs may be filled at high water, though the tides are rather inconvenient than advantageous to brine-pits. 2dly. The brine-pits, properly so called, which are divided into a number of compartments by means of little banks. All these compartments have a communication with each other, but so that the water frequently has a long circuit to make, from one set to another. Sometimes it must flow 400 or 500 yards, before it reaches the extremity of this sort of labyrinth. The various divisions have a number of singular names, by which they are technically distinguished. They should be exposed to the north, north-east, or north-west winds. The water of the sea is let into these reservoirs in the month of March, where it is exposed on a vast surface to evaporation. The first reservoir is intended to detain the water till its impurities have subsided, and from it the other reservoirs are supplied, as their water evaporates. The salt is considered to be on the point of crystallizing when the water begins to grow red. Soon after this, a pellicle forms on the surface, which breaks, and falls to the bottom. Sometimes the salt is allowed to subside in the first compartment; at others, the strong brine is made to pa on to the others, where a larger surface is exposed to the air. In either case the salt is drawn out, and left upon the borders to drain and dry. The salt thus obtained, partakes or the colour of the bottom on which it is formed; and is hence white, red, or gray. Sea water contains, in 1000 parts, 25 of chloride of sodium, 5·3 sulphate of magnesia, 3·5 chloride of magnesium, 0·2 carbonate of lime and magnesia, 0·1 sulphate of lime, besides 1 ⁄ 2000 of sulphate and muriate of potash. It also contains iodide of sodium, and bromide of magnesium. Its average spec. grav. is from 1·029 to 1·030. IMG:4147767755307473660_illo1088.png:Graduation house Figs. 962-964 enlarged (155 kB) Sea-water and weak brines may be concentrated either by the addition of rock salt, by spontaneous evaporation in brine-pits (see suprà ), or by graduation. Houses for the last purpose are extensively employed in France and Germany. The weak brine is pumped into an immense cistern on the top of a tower, and is thence allowed to flow down the surface of bundles of thorns built up in regular walls, between parallel wooden frames. At Salza, near Schönebeck, the graduation-house is 5817 feet long, the thorn walls are from 33 to 52 feet high, in different parts, and present a total surface of 25,000 square feet. Under the thorns, a great brine cistern, made of strong wooden planks, is placed, to receive the perpetual shower of water. Upon the ridge of the graduation-house there is a long spout, perforated on each side with numerous holes, and furnished with spigots or stopcocks for distributing the brine, either over the surface of the thorns, or down through their ma ; the latter method affording larger evaporation. The graduation-house should be built lengthwise in the direction of the prevailing wind, with its ends open. An experience of many years at Salza and Dürrenberg has shown, that in the former place graduation can go on 258, and in the latter 207 days, on an average, in the year; the best season being from May till August. At Dürrenberg, 3,596,561 cubic feet of water are evaporated annually. According to the weakne of the brine, it must be the more frequently pumped up, and made to flow down over the thorns in different compartments of the building, called the 1st, 2d, and 3d graduation. A deposit of gypsum incrusts the twigs, which requires them to be renewed at the end of a certain time. Figs. 962. and 963. represent the graduation-house of the salt-works at Dürrenberg. a , a , a , are low stone pillars for supporting the brine cistern b , called the soole-schiff . c , c are the inner, d , d the outer, walls of thorns; the first have perpendicular sides, the last sloping. The spars e , e , which support the thorns, are longer than the interval between two thorn walls from f to g , fig. 963 , whereby they are readily fastened by their tenons and mortises. The spars are laid at a slope of 2 inches in the foot, as shown by the line h , i . The bundles of thorns are each 1 1 ⁄ 2 foot thick, from 5 to 7 feet long, and are piled up in the following way:——Guide-bars are first placed in the line k , l , to define the outer surface of the thorn wall, the undermost spars m , n , are fastened upon them; and the thorns are evenly spread, after the willow-withs of the bundles have been cut. Over the top of the thorn walls are laid, through the whole length of the graduation-house, the brine spouts o , o , which are secured to the upper beams; and at both sides of these spouts are the drop-spouts p , p , for discharging the brine by the spigots s , s , as shown upon a larger scale in fig. 964. The drop-spouts are 6 feet long, have on each side small notches, 5 inches apart, and are each supplied by a spigot. The space above the ridge of the graduation-house is covered with boards, supported at their ends by binding-beams q . r , r show the tenons of the thorn-spars. Over the soole schiff b , inclined planes of boards are laid for conducting downwards the innumerable showers. The brine, which contains at first 7·692 per cent. of salt, indicates, after the first shower, 11·473; after the second, 16·108; and after the third, 22. The brine, thus concentrated to such a degree as to be fit for boiling, is kept in great reservoirs, of which the eight at Salza, near Schönebeck, have a capacity of 2,421,720 cubic feet, and are furnished with pipes leading to the sheet-iron salt-pans. The capacity of these is very different at different works. At Schönebeck there are 22, the smallest having a square surface of 400 feet, the largest of 1250, and are enclosed within walls, to prevent their being affected by the cold external air. They are covered with a funnel-formed or pyramidal trunk of deals, ending in a square chimney, to carry off the steam. IMG:4147767755307473660_illo1089.png:Salt-pan Figs. 965-967 enlarged (227 kB) Figs. 965 , 966 , 967. represent the construction of a salt-pan, its furnace, and the salt store-room of the works at Dürrenberg; fig. 967. being the ground plan, fig. 966. the longitudinal section, and fig. 965. the transverse section, a is the fire-grate, which slopes upwards to the back part, and is 31 1 ⁄ 2 inches distant from the bottom of the pan. The ratio of the surface of the grate to that of the bottom of the pan, is as 1 to 59·5; that of the air-hole into the ash-pit, as 1 to 306. The bed under the pan is laid with bricks, smoothly plastered over, from b to c , in fig. 966. Upon this bed the pillars d , d , ., are built in a radiated direction, being 6 inches broad at the bottom, and tapering to 1 1 ⁄ 2 inch at top. The pan is so laid that its bottom has a fall towards the middle of 2 1 ⁄ 2 inches: see e , f , fig. 966. The fire diffuses itself in all directions under the pan, proceeds thence through several holes g , g , g , into flues h , h , h , which run round three sides of the pan; the burnt air then pa es through i , fig. 967. , under other pans, from which it is collected in the chimneys k , k , to be conducted into the drying-room. At l , l , there is a transverse flue, through which, by means of dampers, the fire-draught may be conducted into an extra chimney m . From the flues k , k , four square iron pipes n , n , i ue and conduct the burnt air into the main chimneys in the opposite wall. The bottoms of the several flues have a gradual ascent above the level of the fire-grate. A special chimney o , rises above the ash-pit, to carry off the smoke, which may chance to regurgitate in certain states of the wind. p , p , are iron pipes laid upon each side of the ash-pit (see figs. 966. and 967. ), into which cold air is admitted by the flue q , r , where, becoming heated, it is conducted through iron pipes s , and thence escapes at t , into the stove-room. Upon both sides of the hot flues in the stove-room, hurdle-frames u , u , are laid, each of which contains 11 baskets, and every basket, except the undermost, holds 60 pounds of salt, spread in a layer 2 inches thick. v , v , show the pipes by which the pan is supplied with graduated brine. Description of the Steam-trunk, in fig. 968. IMG:4147767755307473660_illo1090.png:Stram-trunk In front of the pan a , a , there are two upright posts, upon which, and in holes of the back wall, two horizontal beams b , b , are supported. The pillars c , c , are sustained upon the bearers d , d . At e , e , a deep quadrangular groove is made in the beams, for fixing down the four boards which form the bottom of the steam-way. In this groove any condensed water from the steam collects, and is carried off by a pipe f , to prevent it falling back into the pan. Upon the three sides of the pan not in contact with the wall, there are three rows of boards hinged upon planks b , b . Behind the upper one, a board is hung on at g , upon which the boiled salt is laid to drain. The two other rows of boards are hooked on so as to cover the pan, as shown at h . Whenever the salt is sufficiently drained, the upper shelves are placed in a horizontal position; the salt is put into small baskets, and carried into the stove-room. i , k , is the steam-trunk; l , m , is a tunnel for carrying off the steam from the middle of the pan, when this is uncovered by lifting the boards. In proportion as the brine becomes concentrated by evaporation, more is added from the settling reservoir of the graduation-house, till finally small crystals appear on the surface. No more weak brine is now added, but the charge is worked off, care being taken to remove the scum, as it appears. In some places the first pan is called a schlot-pan, in which the concentration is carried only so far as to cause the deposition of the sludge, from which the saline solution is run into another pan, and gently evaporated, to produce the precipitation of the fine salt. This salt should be continually raked towards the cooler and more elevated sides of the pan, and then lifted out with cullender-shovels into large conical baskets, arranged in wooden frames round the border of the pan, so that the drainage may flow back into the boiling liquor. The drained salt is transferred to the hurdles or baskets in the stove-room, which ought to be kept at a temperature of from 120° to 130°, Fahr. The salt is then stowed away in the warehouse. The graduation range should be divided lengthwise into several sections: the first to receive the water of the spring, the lake, or the sea; the second, the water from the first shower-receiver; the third, the water from the second receiver; and so on. The pumps are usually placed in the middle of the building, and lift the brine from the several receivers below into the alternate elevated cisterns. The square wooden spouts of distribution may be conveniently furnished with a slide-board, attached to each of their sides, to serve as a general valve for opening or shutting many trickling orifices at once. The rate of evaporation at Moutiers is exhibited by the following table :— | Number of Showers. | Total Surface of the Fagots. | Specific Gravity of the Brine. | Water evaporated. | | 1·010 | 0·000 | | 1 and 2 | 5158 | square feet | 1·023 | 0·540 | | 3, 4, 5, 6, 7, 8, and 9 | 2720 | | 1·072 | 0·333 | | 10 | 550 | | 1·140 | 0·062 | | Total evaporation | 0·935 | | Water remaining in the brine at the density of 1·140 | 1·065 | | Water a igned at the density of 1·010 | 1·000 | From the above table it appears that no le than 10 falls of the brine have been required to bring the water from the specific gravity 1·010 to 1·140, or 18° Baumé. The evaporation is found to proceed at nearly the same rate with the weaker water, and with the stronger, within the above limits. When it arrives at a density of from 1·140 to 1·16, it is run off into the settling cisterns. M. Berthier calculates, that upon an average, in ordinary weather, at Moutiers, 60 kilogrammes of water (13 gallons, imp.) are evaporated from the fagots, in the course of 24 hours, for every square foot of their surface. Without the aid of currents of air artificially warmed, such an amount of evaporation could not be reckoned upon in this country. In the schlotting , or throwing down of the sediment, a little bullock’s blood, previously beaten up with some cold brine, promotes the clarification. When the brine acquires, by brisk ebullition, the density of 1·200, it should be run off from the preparation, to the finishing or salting pans. The mother-water contains a great deal of chloride of magnesium, along with chloride of sodium, and sulphate of magnesia. Since the last two salts mutually decompose each other at a low temperature, and are transformed into sulphate of soda, which crystallizes, and muriate of magnesia, which remains di olved, the mother-water with this view may be exposed in tanks to the frost during winter, when it affords three succe ive crystalline deposits, the last being sulphate of soda, nearly pure. The chloride of magnesium, or bittern, not only deteriorates the salt very much, but occasions a considerable lo of weight. It may, however, be most advantageously got rid of, and converted into chloride of sodium by the following simple expedient:—Let quicklime be introduced in equivalent quantity to the magnesia present, and it will precipitate this earth, and form chloride of calcium, which will immediately react upon the sulphate of soda in the mother-water, with the production of sulphate of lime and chloride of sodium. The former being sparingly soluble, is easily separated. Lime, moreover, decomposes directly the chloride of magnesium, but with the effect of merely substituting chloride of calcium in its stead. But in general there is abundance of sulphate of soda in brine springs to decompose the chloride of calcium. A still better way of proceeding with sea-water, would be to add to it, in the settling tank, the quantity of lime equivalent to the magnesia, whereby an available deposit of this earth would be obtained, at the same time that the brine would be sweetened. Water thus purified may be safely crystallized by rapid evaporation. In summer, the saturated boiling brine is crystallized by pa ing it over vertical ropes; for which purpose 100,000 metres (110,000 yards) are mounted in an apartment 70 metres (77 yards) long. When the salt has formed a crust upon the ropes about 2 1 ⁄ 2 inches thick, it is broken off, allowed to fall upon the clean floor of the apartment, and then gathered up. The salting of a charge, which would take 5 or 6 days in the pan, is completed in this way in 17 hours; but the mother-waters are more abundant. The salt is, however, remarkably pure. The boilers constructed at Rosenheim, in Bavaria, evaporate 3 1 ⁄ 2 pounds of water for every pound of wood burned; which is reckoned a favourable result; but some of those described under Evaporation , would throw off much more. “The rock salt mines and principal brine springs are in Cheshire; and the chief part of the Cheshire salt, both fo il and manufactured, is sent by the river Weaver to Liverpool, a very small proportion of it being conveyed elsewhere, by canal or land carriage. There are brine springs in Staff ords hire, from which Hull is furnished with white salt; and in Worcesters hire, from which Gloucester is supplied. If to the quantity shipped by the Weaver, 100,000 tons of white salt are added annually for internal consumption and exports, exclusive of Liverpool, the total manufacture will be approached very nearly; but as there is now no check from the excise, it is impo ible to ascertain it exactly. Fo il salt is used in small quantities at some of the Cheshire manufactories, to strengthen the brine, but is principally exported; some to Ireland, but chiefly to Belgium and Holland.” [52] The average quantity of rock salt sent annually down the river Weaver, from the mines in Cheshire, between the years 1803 and 1834 inclusive, was 86,000 tons, of 2,600 lbs. each; the greatest being 125,658, in the year 1823, and the least 47,230, in the year 1813. The average quantity of white salt sent annually down the Weaver from the manufactories in Cheshire during the same period, was 221,351; the greatest being 383,669, in the year 1832, and the least being 120,486, in the year 1811. [52] Tables of the Revenue, Population, Commerce, ., for 1836, p. 122. M. Clement-Desormes, engineer and chief actionnaire of the great salt-works of Dieuze, in France, informs me that the internal consumption of that kingdom is rather more than 200,000 tons per annum, being at the rate of 6 1 ⁄ 2 kilogrammes for each individual of a population estimated at 32,000,000. As the retail price of salt in France is 10 sous per kilogramme (of 2 1 ⁄ 5 lbs. avoird.), while in this country it is not more than 2 sous (1 penny), its consumption per head will be much greater with us; and, taking into account the immense quantity of salted provisions that are used, it may be reckoned at 22 lbs.; whence our internal consumption will be 240,000 tons, instead of 100,000, as quoted above, from the tables published by the Board of Trade. In 1836, 9,622,427 bushels, of 56 lbs. = 240,560 tons of salt, value 173,923 l. , were exported from the United Kingdom, of which 1,350,849 bushels went to Ru ia; 1,235,086 to Belgium; 314,132 to the Western coast of Africa; 1,293,560 to the British North American colonies; 2,870,808 to the United States of America; 53,299 to New South Wales, Van Diemen’s Land, and other Australian settlements; 58,735 to the British West Indies; and 90,655 to Guernsey, Jersey, Alderney, and Man. SAND (Eng. and Germ.; Sable , Fr.); is the name given to any mineral substance in a hard granular or pulverulent form, whether strewed upon the surface of the ground, found in strata at a certain depth, forming the beds of rivers, or the shores of the sea. The siliceous sands seem to be either original crystalline formations, like the sand of Neuilly, in 6-sided prisms, terminated by two 6-sided pyramids, or the débris of granitic, schistose, quartzose, or other primitive crystalline rocks, and are abundantly distributed over the globe; as in the immense plains known under the names of downs, deserts, steppes , landes , ., which, in Africa, Asia, Europe, and America, are entirely covered with loose sterile sand. Valuable metallic ores, those of gold, platinum, tin, copper, iron, titanium, often occur in the form of sand, or mixed with that earthy substance. Pure siliceous sands are very valuable for the manufacture of gla , for making mortars, filters, ameliorating dense clay soils, and many other purposes. For moulder’s sand, see Founding . Lynn and Ryegate furnish our purest siliceous sand. SANDAL or RED SAUNDERS WOOD ( Santal Fr.; Sandelholz Germ.); is the wood of the Pterocarpus santalin us , a tree which grows in Ceylon, and on the coast of Coromandel. The old wood is preferred by dyers. Its colouring matter is of a resinous nature; and is, therefore, quite soluble in alcohol, e ential oils, and alkaline lyes; but sparingly in boiling water, and hardly if at all in cold water. The colouring matter which is obtained by evaporating the alcoholic infusion to dryne , has been called santa line ; it is a red resin, which is fusible at 212° F. It may also be obtained by digesting the rasped sandal wood in water of ammonia, and afterwards saturating the ammonia with an acid. The santa line falls, and the supernatant liquor, which is yellow by transmitted, appears blue by reflected light. Its spirituous solution affords a fine purple precipitate with the pro to chloride of tin, and a violet one with the salts of lead. Santa line is very soluble in acetic acid, and the solution forms permanent stains upon the skin. Sandal wood is used in India, along with one-tenth of sapan wood (the Cæsalpinia sapan of Japan, Java, Siam, Celebes, and the Philippine isles), principally for dyeing silk and cotton. Trommsdorf dyed wool, cotton, and linen a carmine hue by dipping them alternately in alkaline solution of the sandal wood, and in an acidulous bath. Bancroft obtained a fast and brilliant reddish-yellow, by preparing wool with an alum and tartar bath, and then pa ing it through a boiling bath of sandal wood and sumac. Pelletier did not succeed in repeating this experiment. According to Togler, wool, silk, cotton, and linen, mordanted with salt of tin, and dipped in a cold alcoholic tincture of the wood, or the same tincture mixed with 8 parts of boiling water, become of a superb ponceau-red colour. With alum, they took a scarlet-red; with sulphate of iron, a deep violet, or brown-red. Unluckily these dyes do not stand exposure to light well.