Scientific American Supplement, No. 458, October 11, 1884 eBook

This eBook from the Gutenberg Project consists of approximately 150 pages of information about Scientific American Supplement, No. 458, October 11, 1884.

Scientific American Supplement, No. 458, October 11, 1884 eBook

This eBook from the Gutenberg Project consists of approximately 150 pages of information about Scientific American Supplement, No. 458, October 11, 1884.
is drawn out of the earth and its level is depressed, so that the upper malarious strata, exposed to the direct action of the air, are deprived of moisture during the hot season.  This system of drainage is not a modern invention; the Italian monks understood it as well as, and even better than, we do.  In deep and loose soils they used sometimes, just as we do now, porous clay pipes; but when the subsoil was formed of compact and nearly impermeable matters, they employed a system of drainage, the extent and grandeur of which astonishes us.  It is that of drainage by cavities, applied by the Etruscans, Latins, and Volsci to all the Roman hills formed of volcanic tufa, the tradition of which I have found still preserved in some countries of the Abruzzi.

We may sometimes establish a double drainage, from below and from above; that is to say, to drain the subsoil, and at the same time increase the evaporation of water from the surface of the ground.  It is well known that clearing off the forests of malarious countries has often proved an excellent means of making lands salubrious which were before too damp; for, by removing every obstacle to the direct action of the sun’s rays upon the ground, we cause an increase of evaporation from its surface, and may thus be enabled to exhaust the superficial strata completely of their water during the hot season.  In very moist lands, which lend themselves readily to deep drainage, the combination of the latter with a clearing of the surface has, in almost every quarter of the globe, rendered possible a very widespread and sometimes a quite lasting freedom from malaria.  But, although a nearly universal experience proclaims this fact, there is a school which, following in the footsteps of Lancisi, maintains the contrary opinion, that it is necessary to preserve the forests in malarious districts, and even to increase their extent, since the trees filter the infected atmosphere and arrest the malaria in their foliage.  This strange theory was formulated by Lancisi in 1714, on the occasion of the proposed clearing of a forest belonging to the Caetani family, and lying between the Pontine Marshes and the district of Cistema.  Lancisi was completely imbued with the paludal notion, and consequently believed that the very severe malaria of Cistema was brought by the winds from the coast marshes, instead of being produced in the soil surrounding the district, which was then covered by this forest.  He believed then that the forest acted as a protective rampart, and he prevented its being cut down.  But toward the middle of the present century the Caetani had the woods cleared off from the entire belt of land surrounding Cistema.  Twenty years later I was able to show that Cistema had gained greatly in salubrity.  I published my observation in 1879, and, naturally, was taken to task rather sharply in the name of the sacred tradition.  Happily these recriminations led our Minister of Agriculture to have the question

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Scientific American Supplement, No. 458, October 11, 1884 from Project Gutenberg. Public domain.