CHAPTER V. TESTIMONY OF WATER. Religion and Chemistry | ||
5. CHAPTER V.
TESTIMONY OF WATER.
THE atmosphere, as you will remember, consists mainly of two permanent and elementary gases; and having discussed the functions of its active element, oxygen, it would seem natural to consider next the offices of nitrogen, that most singularly inert gas, which constitutes no less than four-fifths of its whole mass; but we shall understand more clearly the complicated relations of this truly wonderful substance, associated as it is with all the higher forms of corporeal vitality, after we are acquainted with two of the remarkable cycles in nature, in which the water and carbonic dioxide of the atmosphere play a conspicuous part. It is true that these two substances are very variable constituents, and make up at best only an exceedingly small fraction of the whole mass of the air; but nevertheless, they discharge functions no less important than those of oxygen and nitrogen, and we shall find that they are equally rich in illustrations of the wisdom and power of God.
I have already alluded to the fact that the most striking illustrations of creative wisdom have been
The condition of the atmosphere of aqueous vapor, which surrounds the globe, differs essentially from that of the more permanent gases which are simultaneously present. Oxygen and nitrogen cannot be reduced to liquids even by the intense cold at the poles. It is very different with aqueous vapor. The slightest reduction of temperature, when the air is saturated with moisture, is sufficient to condense a portion of the vapor to water, and to shower it on the earth in drops of rain. On the other hand, when the temperature rises, the heat converts more water into vapor, and the aqueous atmosphere is replenished. Thus it is that the
I stated in the last lecture that our atmosphere may be regarded as made up of three partial atmospheres, simultaneously surrounding the globe, and as was the case with the atmosphere of oxygen, we shall best understand the fluctuations of the aqueous atmosphere if we begin by eliminating, for a moment, from our thoughts the other two. In order to make the subject clear, it will be necessary for me to dwell very briefly on a few well established facts in meteorology, which, although not very interesting in themselves, will unfold to us some of the beautiful provisions of nature by which the aqueous circulation of the globe is maintained.
If there were no free oxygen or nitrogen gas, the earth would still be surrounded with an atmosphere of aqueous vapor, and we are able to foresee, in some small measure, what the conditions of such an atmosphere would be. Its density at the sea level would depend chiefly on the temperature, and would therefore vary very rapidly with the latitude, and would be constantly changing at the same locality with the alternations of the climate. We are able to determine approximately what the density would be at any given temperature, and a few of the results are included in the following table:
Temperature. | Weight. |
Fahrenheit. | Grains. |
0° | 0.78 |
10° | 1.11 |
20° | 1.58 |
30° | 2.21 |
40° | 3.09 |
50° | 4.28 |
60° | 5.87 |
70° | 8.00 |
80° | 10.81 |
90° | 14.50 |
It is evident from these numbers, that a very small change of temperature would cause immense fluctuation in such an atmosphere. At 0° one cubic foot of the aqueous atmosphere could contain only about three-fourths of a grain of vapor, while at 80° it could contain fifteen times as much, and hence, although under the tropics the density of our assumed atmosphere would be comparatively large, there would be almost a complete vacuum at the poles. Into this vacuum the vapor would flow from the equator, and thus in either hemisphere there would result a perfect torrent of vapor rushing towards the North or South. But it is also evident that, as this current became chilled in passing through the cooler climate of the temperate zone, the vapor would gradually condense to water, which, falling on the land or on the ocean, would return in time to the equator, ready to begin again the same succession of ceaseless changes.
Although the presence of the air materially modifies, it does not essentially change, the aqueous circulation. The air retards the formation of vapor, but does not prevent it, and at any given temperature the same amount of water will evaporate into
Were there no air on the globe, the quantity of vapor would adjust itself almost instantaneously to any variation of temperature, and the maximum amount possible would always be present at any given place. An elevation of temperature would be attended by rapid evaporation, and the amount of water required to fill the space would suddenly flash into vapor; while, on the other hand, a corresponding depression of temperature would be accompanied with an equally sudden precipitation of the excess of water which the air could no longer contain, not in genial showers or diffusive rain, but in terrific torrents, of which the deluging showers of the tropics can give us only a feeble conception; for the drops, falling without resistance, would be as destructive in their effects as volleys of leaden shot.
In the actual condition of the atmosphere, the presence of a dense medium very greatly retards these changes, and although it does not alter their essential nature, it moderates their action and mitigates the violence of their effects. An elevation of
Again, the presence of the air very greatly retards the aqueous circulation above described, without altering its essential character. There is now the same great difference between the density of the atmosphere of vapor at different latitudes, as if it were the only atmosphere on the globe, and the dense vapor of the tropics tends constantly to flow towards either pole; but as it cannot move without carrying with it the whole mass of the atmosphere, this tendency merely increases the velocity of those great aerial currents, already described in a previous lecture. Still the general fact remains the same. From the whole surface of the globe water is constantly evaporating into the aqueous atmosphere which surrounds it. The heated air from the tropics, heavily charged with moisture, is continually moving towards the colder regions, both of the North and of the South; and as the current thus becomes chilled, the vapor is slowly condensed, and the water showered down in fertilizing rains on the land. Thus it is that those beautiful provisions which we see in the rain all depend on the presence of the air, and result from a careful adjustment of the properties of aqueous vapor to the exact density of our atmosphere. "Hath the rain a Father?'' Science, by discovering these evidences of skilful adaptation,
But what becomes of the rain? Would that I could answer this question satisfactorily. We all understand the general theory of the aqueous circulation, but the deepest philosophy and the keenest science are not able to fathom its details, or to comprehend in their fulness the world of wonderful adaptations which the question unfolds. We all know that the drops of rain percolate through the soil, and collect in natural reservoirs formed between the layers of rock, and that these reservoirs supply the springs. The rills from numerous adjacent springs unite to form a brook, which increases as it flows, until it finally becomes the majestic river, rolling silently on its course. Every drop of that water has been an incessant wanderer since the dawn of creation, and it will soon be merged again in the vast ocean, only to begin anew its familiar journey. If you would gain an idea of the magnitude and extent of this wonderful circulation, you must bring together, in imagination, all the rivers of the world, the Amazon and the Orinoco, the Nile and the Ganges, the Mississippi and the St. Lawrence, and, adding to these the ten thousands of lesser streams, endeavor to form a conception of the incalculable amount of water which during twenty-four hours they pour into the vast basin of the world, and then remember that during the same period at least four times as much
In order that we may appreciate, in some humble measure, the force of this evidence, let us consider
It is a familiar fact, that water is an essential condition of organic life; but few persons, I suspect, are aware that this familiar liquid constitutes the greater part of all organized beings. The physical man has been described by one writer as consisting of merely a few pounds of solid matter distributed through six pailfuls of water, and it is a fact that no less than four-fifths of these bodies of ours are made up of water. Yet this is a small proportion compared with the amount which enters into the structure of most of the lower animals. Some of these, such as the medusæ,—sunfishes,—are little else than organized water. Professor Agassiz obtained from one of the large sunfishes found on our coast, weighing thirty pounds, only two hundred and forty grains of solid matter; and we may safely say that at least nine hundred and ninety-nine parts in a thousand of these singular animals consist of water. Water constitutes, to almost as great an extent, most of the vegetable products which are articles of food, as will be seen by the accompanying table.
Plums | contain 75 per cent. of water. |
Potatoes | " 75 " " " |
Apples | " 80 " " " |
Carrots | " 83 " " " |
Turnips | " 90 " " " |
Watermelons | " 94 " " " |
Cucumbers | " 97 " " " |
It is evident from these facts that water is the
"The mountain chains,'' writes Professor Guyot, in his excellent work Earth and Man, "are great condensers, placed here and there along the continents to rob the winds of their treasures, and to serve as reservoirs for the rain-waters, and to distribute them afterwards as they are needed over the surrounding plains. Their wet and cloudy summits are untiringly occupied with this important work, and from their sides flow numberless torrents and rivers, carrying in all directions wealth and life.''
Thus the mountains, whose majestic forms affect so powerfully the human soul, and which have exerted such an influence on the history of the race, are also among the most beneficent means in the Divine Providence by which the earth has been fertilized and rendered a fit abode for man. Moreover, these mountain chains have been evidently so distributed
But it is not the mountains alone which condense the vapor of the atmosphere; for, under certain conditions, the level plains act in a similar way, and distil the precious drops of dew upon field and meadow, distributing it among the plants with discriminating care for the necessities of each. The dew is simply another phase of the great aqueous circulation, and, like the rain, it is a persuasive witness of the Divine Disposer, who has adjusted its amount to the wants of the vegetable world. Every one has noticed the deposition of moisture on a pitcher of ice-cold water during a summer's day, and in this familiar fact, we have at once an example and an illustration of the simple provision by which, during even the long droughts of summer, the plants receive a partial supply of water, sufficient, at least, to sustain their life until the later rains bring the autumn fruits to maturity, and stimulate a more vigorous growth.
The explanation of the dew upon the pitcher is very simple. The layer of air in contact with its cold mass is rapidly cooled, and when it can no longer hold all the moisture it contains, the excess is deposited in drops on the surface. Exchange now the pitcher for the earth, and you have at once an explanation of the proximate cause of the dew. After sunset the earth, like the pitcher, cools down the layer of atmosphere immediately in contact with it to such a degree that the whole of the vapor can no longer retain its aeriform condition. As a necessary result, a portion is condensed and deposited upon the surface, and this is what we call dew. But it will be asked, What cools the earth so suddenly after the setting of the sun? For this is not so evident as the cause of the coldness of the pitcher. Certainly not, and the question will lead us to a study of those relations in which the adaptations to be discovered in this natural phenomenon are chiefly to be found.
The earth, as I stated in the second lecture, is moving with immense rapidity through a space whose temperature is at least 270 degrees below the zero of Fahrenheit's thermometer, and, like a heated cannon-ball hung in the middle of a cold room, it is continually losing heat by radiation. The dense atmosphere with which it is enveloped, acting, as we have seen, like a blanket, protects the earth from the intense cold of space to a certain extent; but still the constant loss of heat is so great, that, were the sun's rays withheld for a few days, the temperature of the surface-land, even in the tropics, would fall as low as it is now at the poles during the long night
You must all have noticed that the most copious deposition both of dew and frost takes place on clear nights, and that during cloudy weather this supply of moisture is entirely withheld. The reason is obvious. The earth loses heat by radiation, and the clouds, intercepting the rays, reflect them back to the earth. A shed or any other protection spread over the ground acts in the same way, and it is well known that a covering, however slight, is sufficient to protect tender plants from the blight of the early frosts. Can it then be an accident, a mere result of chance, that the dew is deposited most abundantly where it is needed most, and that this supply of moisture fails only when the clouds promise a more copious draught of liquid nourishment from the rain?
There is still another fact presented by the dew which is equally suggestive. The heavens do not distil their liquid treasures upon all objects alike, but the dew is deposited much more abundantly on the herbage, the shrubs, and the trees, which need the refreshing moisture, than on fallow land, the sandy plain, or the beaten road; and here again the cause has been discovered. It is evident from the general theory of the subject, that the
It will be remembered, as I stated in the second lecture of this course, that the points of leaves have the power of silently discharging the thunderbolts of heaven, and that, in consequence, every tree acts far more efficiently to avert the stroke of this destructive agent than the best constructed lightning-rod. Is not, now, the force of this evidence of adaptation very greatly enhanced, when we find that the surfaces of these same leaves have been endowed with an equally remarkable power of radiating heat, by which they are insured a daily supply of moisture when they need it most? Could the adaptation of the structure of the leaf to these two entirely distinct
I might, with advantage, enter more into detail in regard to the laws of the distribution both of the rain and of the dew, but time and space forbid. I have been able only to open the subject; yet if I have succeeded in impressing you with the extent of the field which these beautiful phenomena present
Glancing now, for a single moment, at the æsthetic aspects of the subject, consider what sources of pleasure the varied phases of the aqueous circulation furnish, and what an influence on the soul of man they are calculated to exert. The bubbling spring, the purling rill, the murmuring brook, the sparkling cascade, the roaring torrent, the majestically flowing river, are familiar images of poetry, and the occasions of mental emotions which all have experienced and none can fully describe; while the mighty cataract and the ocean-storm are among the sublimest aspects of nature, and inspire the beholder with reverence and awe. When, now, you reflect that the chords of the human soul have been so strung as to vibrate in sympathy with these emotions of the material creation, and that thus the aqueous circulation has been made a means of instructing
The mechanism of nature differs, as we have seen, from the creations of human ingenuity, in the fertility of its resources. Man combines numerous means in order to produce a single end; but in nature the most varied and apparently incompatible results flow from a single design. In God's works the means are employed, not as we use them in the poverty of our resources, but from the exuberance of riches. To use the language of another: "All the means are ends, and all the ends are means;'' and the grand result is an harmonious system, in which every part is a whole, and where the whole that is known is felt to be only a very insignificant part. Such is the character of the aqueous circulation, which we are now studying, and assuredly the numerous results we have already seen flowing from this simple mechanism are sufficient to mark the system as Divine; but we have not as yet exhausted its resources. Indeed, we have been all the time looking at only one side of the design, and there is a whole set of adaptations yet unnoticed, which are no less important in the scheme of organic nature than the one we have chiefly considered. And when we have become acquainted with these, we shall find still other phases of this boundless plan presented to our view, and not until man ceases to learn by study, or the waters cease to roll, will the subject be exhausted.
We have thus far only considered the agency of the aqueous circulation in distributing over the earth the chief constituent of all organic matter, together with some of the secondary ends which the river-system of the globe subserves. But there is another condition of organic life no less essential than moisture. The animal kingdom is absolutely dependent on the vegetable, and plants cannot grow except within a limited range of temperature. Therefore, unless during at least a portion of the year the amount of heat supplied is sufficient to maintain the temperature of the climate within the required limits, organic life cannot exist in that region. Now this familiar substance, water, has been endowed with most remarkable and unusual properties, by which the aqueous circulation has been made a great means of distributing heat, and thus of sustaining organic life in vast tracts of country where otherwise it could not exist; and it is to this class of its adaptations that I wish next to call your attention.
One of the prominent inventions of modern times is the method of heating large buildings by steam. You must all have seen the apparatus. There is first the boiler, where the steam is generated by the combustion of fuel; then pipes, by which it is distributed to the different rooms; next the iron radiators, in which the steam is condensed to water, and during this change gives out heat, which is radiated from the corrugated surface of the iron; and, lastly, the return pipes, through which the condensed water flows back to the boiler, ready to start again on the same journey. Every one is familiar with these
Your attention, perhaps, has been called to the efficiency and economy of this method of heating; you have admired its neatness and absolute safety from fire, and have been delighted with the softness of the temperature which it diffuses through the rooms; or, if you have examined more closely the details of the apparatus, you must have been struck with the ingenuity of the adjustments by which it is self-regulated. Yet this is no new invention. A similar apparatus, on a vastly grander scale, working with far greater economy and efficiency, and provided with adjustments of wonderful delicacy, which perfectly regulate its action, and which never fail and never wear out, has been at work ever since the dawn of the creation, and is at this moment softening the inclemency of our northern winter.
The general aqueous circulation is a great steam-heating apparatus, with its boiler in the tropics and its condensers all over the globe. The sun's rays make the steam, and wherever dew, rain, or snow falls, there the heat, which came originally from the sun, and which has been brought from the tropics concealed in the folds of the vapor, is set free to warm the less favored regions of the earth. This apparatus of nature, although so much simpler, and
Having considered that peculiar quality of vapor through which the aqueous circulation becomes an important means of distributing the sun's heat over the surface of the globe, we might next discuss more at length the extent of its influence, and examine in detail the ingenious system of checks and balances
The amount of heat required to raise the temperature of a pound of water, or of any other substance, one degree, is capable of exact measurement, and the quantity has been determined experimentally for almost every known substance. These experiments have led to a remarkable result, to which I alluded in a former lecture. It appears that, when water is heated through a given number of degrees, it absorbs more than twice as much heat as any other substance (except one or two very closely related bodies), and more than ten times as much as iron and most of the metals. It is not probable that many of my audience have verified this striking result, but you all know how long it takes to boil a tea-kettle, even over a brisk fire, and have, therefore, some conception of the amount of heat which cold water is capable of absorbing. This familiar experience shows that water has a very great capacity of holding heat, and accurate experiment has proved, as just stated, that, with the exception just noticed, water contains, at the same temperature, more than twice as much heat as any other solid or liquid known.
The importance of this simple provision will appear if you reflect that it makes the ponds, the
"On the coast of Cornwall shrubs as delicate as the laurel or the camellia are green through the whole year, while under the same latitude in the interior of the continents, the most hardy trees can alone brave the rigor of the winter. But on the other hand, the mild climate of England cannot ripen the grape, although almost under the same parallel grow the delicious wines of the Rhine. At Astrachan, on the northern shore of the Caspian, as Humboldt tells us, the grapes and fruits of every kind are as beautiful and luscious as in the Canaries and in Italy; the wines have all the fire of those of the south of Europe, although in the same latitude, at the mouth of the Loire, on the Atlantic sea-coast, the vines hardly flourish at all. But while in the south of France the winter is a perpetual spring, the summers of the Caspian are succeeded by a winter of almost polar severity.''
I might multiply illustrations, but these are sufficient to show how the remarkable property of water
This influence of water is very greatly increased by the oceanic currents, which, like the winds, are set in motion by the heat of the sun, and are constantly carrying the warm waters of the tropics toward the poles. One of the most remarkable of these currents is the Gulf-Stream, which flows near our coast, and which diffuses the warm waters of the Caribbean Sea and the Gulf of Mexico over the Northern Atlantic, depositing on the shores of Scotland and Norway the plants and seeds of the tropics. It is solely the heat which these waters bring with them from the equator that has made the island of Great Britain so great a centre of commerce and civilization; for it must be remembered that the latitude of England is the same as that of Labrador, and, were it not for the influence of this ocean current, her soil would be equally desolate and barren. If the configuration of our Western Continent were only so slightly changed as to give a passage to the equatorial current through the present Isthmus of Panama—a change insignificant in comparison with those which have heretofore taken place—"the mountains of Wales and Scotland would become again the abode of glaciers, and civilization would disappear before the invasion of arctic cold.'' [*] So also it is to the enormous mass of heated water which the Gulf-Stream pours into the seas surrounding
But all these provisions for distributing heat over the earth's surface would have been insufficient to maintain organic life in our northern climate, were it not for still another remarkable property with which water has been endowed,—a property even more entirely unique than either of those we have studied, and one which seems to be an exception to the general laws of nature. The familiar cycles of organic life, both in animals and plants, are intimately associated with the succession of the seasons, and this, in its turn, depends on the inclination of the earth's axis to the plane of the ecliptic, and on the great primary laws by which this axis is constantly maintained in a position parallel to itself during the revolution of the planet around the sun. To these fundamental conditions in the formation of the solar system the whole constitution of organic life on the earth has been adjusted; and Dr. Whewell, in his excellent Bridgewater Treatise, has discussed at length the evidences of design which this circumstance affords. It would be foreign to my plan, to consider these evidences here; but, assuming the succession of the seasons as a part of the order of creation, and as a means of adapting a larger portion of the earth's surface to the habitation of organized beings, it is evident that the higher forms of organic life could be sustained in these northern regions only by furnishing
The required protection has been provided by making a most marked exception to the general laws of expansion in the case of water. It is the general law of nature that all substances are expanded by heat and contracted by cold, and water forms no exception to the general rule, except within certain very narrow limits of temperature, shortly to be noticed. Indeed, were it not for the expansion, we could not readily either heat or cool a large mass of liquid matter. All liquids are very poor conductors of heat, and can be heated only by bringing their particles successively in contact with the source of heat. When you set a tea-kettle over a fire, the first effect of the heat is to expand the particles of water resting on the bottom of the kettle, which, being thus rendered specifically lighter, rise, and are succeeded by colder particles, which are heated and rise in their turn; and thus the circulation is established by which all the particles are successively brought in contact with the heated bottom of the kettle, and in the course of time the temperature of the whole mass is raised to the boiling-point. The case is similar when you add ice to a pitcher of water in order to cool it. The water at the top of the pitcher, in contact with the ice is, of course, cooled, and, being thus rendered specifically heavier than the water below, sinks
The cold atmosphere of winter acts upon the ponds and lakes exactly as the ice on the water in the pitcher. They also are cooled from the surface, and a circulation is established by the constant sinking of the chilled water until the temperature falls to 40°. But at this point, still eight degrees above the freezing-point, the circulation stops. The surface-water, as it cools below this temperature, remains at the top, and in the end freezes; but then comes into play still another provision in the properties of water. Most substances are heavier in their solid than in their liquid state; but ice, on the contrary, is lighter than water, and therefore floats on its surface. Moreover, as ice is a very poor conductor of heat, it serves as a protection to the lake, so that at the depth of a few feet, at most, the temperature of the water during winter is never under
If water resembled other liquids, and continued to contract with cold to its freezing-point,—if this exception had not been made, the whole order of nature would have been reversed. The circulation just described would continue until the whole mass of water in the lake had fallen to the freezing-point. The ice would then first form at the bottom, and the congelation would continue until the whole lake had been changed into one mass of solid ice. Upon such a mass the hottest summer would produce but little effect; for the poor conducting power would then prevent its melting, and instead of ponds and lakes we should have large masses of ice, which during the summer would melt on the surface to the depth of only a few feet. It is unnecessary to state that this condition of things would be utterly inconsistent with the existence of aquatic plants or animals, and it would be almost as fatal to organic life everywhere; for not only are all parts of the creation so indissolubly bound together that, if one member suffers, all the other members suffer with it, but moreover, the soil itself would, to a certain extent, share in the fate of the ponds. The soil is always more or less saturated with water, and, under existing conditions in our temperate zone, the frost does not penetrate to a sufficient depth to kill the roots and seeds of plants which are buried under it. But were water constituted like other liquids, the soil would remain frozen to the depth of many feet, and the only effect of the summer's heat would be to
Moreover, this exceptional property is united in water with another quality, which greatly aids in preserving vegetable life during the winter months. We shudder at the thought of snow, but nevertheless it affords a most effectual protection to the soil, forming as warm a covering as would the softest wool. Water in all its conditions has been made a very bad conductor of heat, and snow is ranked with wool among the poorest of conductors. Heat, therefore, cannot readily escape from a snow-covered soil, and thus its temperature is prevented from falling materially below the freezing-point, however great the severity of the season. Notice now, that, when winter sets in and the cold increases to such a degree as to endanger the tender plants, Nature promptly spreads her great frost-blanket over forest, prairie, meadow, and garden alike, so that all may slumber on in safety until the sun returns and melts away the downy covering, when the buds break forth again and the trees put on a new mantle of living green.
This leads me to speak of still another remarkable property of the wonderful liquid we are studying;
I have said that water presents the only well established exception to the laws of expansion by heat, and some writers on natural theology have dwelt on this point as one of great importance to their argument. But I cannot think they are wise; for, to say the least, they rest their argument on our ignorance, and not on our knowledge. It is true that in the present state of science the anomalous expansion of water near the freezing-point seems to be an exception [*] to the general laws of nature; but hereafter this very anomaly may appear to be the natural result of a more general law not yet discovered, or, like the perturbations in the orbits of the planets, may prove to be the strongest confirmation of the very law it now seems to invalidate. Moreover, I do not share in that indefinite dread of natural laws which troubles so many religious minds. To me the laws of nature afford the strongest evidences of the existence of a God, and in their uniformity I see merely the constant action of an omnipresent Creator, who acts with perfect regularity
Water is the most universal solvent known, and there are but few substances which are not, to a greater or less degree, dissolved by it. Those which we call insoluble generally differ from the rest only in degree. Thus, all lime rocks dissolve to a limited extent in spring water, and the same is also true of almost all mineral substances. The magnificent crystals which we frequently find in the rocks are formed in almost every case by a deposition of the mineral substance from a state of solution in water. The feeble solvent power of the water for these substances is made up by the large volume of the solution, and the length of time occupied in the process of crystallization. Many of the large crystals which may be seen in cabinets of minerals have
Again, the solvent power of water extends to aeriform as well as to the solid substances, so that the gases composing the air pervade the lakes and the oceans as well as the atmosphere. Indeed, it is on the gases dissolved in the water that all the aquatic plants and animals live, and the members of the various finny tribes breathe the free oxygen dissolved in the water, as we breathe the oxygen of the air. Again, the process of respiration is essentially the same with these lower animals that it is with us, and the structure of their organs has been adjusted to the amount of this life-sustaining element which water is capable of dissolving. Moreover, the power which water possesses of dissolving oxygen is much greater than its power of dissolving nitrogen, and hence the air dissolved in the ocean is proportionally much richer in oxygen than our atmosphere. This is undoubtedly another quality with which water has been endowed in order to render the oceans, the lakes, and the rivers a fit habitation for that world of organic life which modern zoölogy has revealed. That we are unable to trace all its relations, is evidently owing to the imperfection of our knowledge. But here a new field of study opens before us, which, when fully explored,
It is not, however, merely as a solvent, that water is an important agent in the great laboratory of the world. I have already stated to what extent all animal and vegetable substances are composed of water, and that some, such as the jelly-fishes among animals, and the gourd family among plants, may be said to be living forms of water. But we should entertain a very erroneous conception of the condition of the water in these animal and vegetable structures, were we to regard it as so much dead material, building up the form like the bricks in an edifice. This water is in constant circulation, conveying nourishment to all the parts, and at the same time removing from the system those tissues which have fulfilled their functions and become effete. It is being constantly decomposed, and as rapidly again reformed, assuming the most protean conditions, and administering to the functions of the animal economy in a thousand ways.
As a constituent of inorganic matter, water is no less important than it is in organized being. A substance so bland as water, and apparently so entirely inactive, which fills the most delicate vegetable cells, and penetrates the finest capillaries of the body,—whose minuteness and delicacy no art can approach, nor imagination scarcely conceive,—yet without affecting either in the slightest degree, we should suppose would be endowed with no affinities, and capable of exerting no chemical force. Yet what is the fact? In attempting to classify
When, lastly, we consider the composition of water, our wonder is still further increased; for it
What a revelation of power we have here! In every drop of water there is a constant striving of the elements to escape; they are exerting a force to break the bonds that unite them, which can be
It is a very common mistake to suppose that the grand in nature is to be seen only in its great water-falls and its lofty mountains; for, to the intellectual eye, there is more real grandeur, more evidence of omnipotence, in a single raindrop than in the rush of Niagara or in the magnitude of Mont Blanc. The more I study the evidence of design in this simple liquid, the more I find there is to learn, and I feel the utter inadequacy of any language to convey the full and complete idea. Review, for a moment, the examples of adaptation which have been so briefly noticed. Remember that water is the liquid of our globe, and the only liquid which exists in any abundance
It is well known that in a mass of air charged with aqueous vapor, the tension of the vapor is added to the tension of the air, and that such a mixture is lighter than a mass of dry air of the same temperature, whose tension equals the united tension of the gas and vapor. If, now, the vapor in such a mass of air is condensed to water dust, whose particles are mutually repelled by their similar electrical charges, we may conceive that the electrical tension takes the place of the tension of the vapor, so that the resulting cloud, as a whole, may be as light as the surrounding atmosphere in which it floats.
CHAPTER V. TESTIMONY OF WATER. Religion and Chemistry | ||