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NJDEP - NJGS - First Annual Report of the Geological Survey of the ...

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' , In <strong>the</strong> use <strong>of</strong> lime as a' fertilizer, it may be established as ageneral rule, that it is only to such lahds that it should be appliedin its caustic state.* ., _hel[ma_l_ ei<strong>the</strong>r alone or eomposted with peat and muck,may be advantageously used in' large qaantities on clayey,sandy, and loamy soils. The principal object in compostingit with peat and muck is, at <strong>the</strong> same time, to" add organicmatter to <strong>the</strong> soil. If <strong>the</strong> soil contains already a sufficientquantity <strong>of</strong> organic matter in an active or proper state, it maybc applied alone. Its mechanical action on many soiIs, particularlyon hardpan, or clayey soilsl rerldbring <strong>the</strong>m mornpulverulent and open, is <strong>of</strong> great importance. It.may beadvantageouslyemployed upon polsonous soils. Copperas orsulphate <strong>of</strong> zrou renders laud sterile. Whenever a soil is derivedfrom <strong>the</strong> debris <strong>of</strong> a rock wherein is found iron pyrites,(sulphuret <strong>of</strong> iron,) it will contain sulphate <strong>of</strong> iron, _tnd very<strong>of</strong>ten in sufficient quantities to destroy vegetation. An in.stance'<strong>of</strong> this was observed in Frankford Township, near <strong>the</strong> ZCounty Poor House. In its vicinity was a ridge <strong>of</strong> slate containinga large amount <strong>of</strong> pyrites, which, being very s<strong>of</strong>_ iscdnstantly undergoing decomposition, and forming sulphate <strong>of</strong>iron, and this is carried over <strong>the</strong> soil and mingled with it by<strong>the</strong> wash <strong>of</strong>'<strong>the</strong> ridge. ,To a calcareous soil, or one which has been formed from <strong>the</strong>debris <strong>of</strong> limestone rock, it may 'be applied in small quantitiesalone I or eomp0sted with large quantities <strong>of</strong> vegetable matter.On <strong>the</strong> northwestern slope <strong>of</strong>' <strong>the</strong> Blue, or Kittatinny Mountaifi,<strong>the</strong> course <strong>of</strong> <strong>the</strong> Little FJatkill is near <strong>the</strong> dividing lineb/_.tweea <strong>the</strong> limestone <strong>of</strong> <strong>the</strong> Heldcrberg Series, and <strong>the</strong> redsandstone and shales <strong>of</strong> <strong>the</strong> Medina' Sandstone. The soil onth e limestone hills between <strong>the</strong> Little 1_'latkitl and <strong>the</strong> Delaware• By caustic llme, is understood <strong>the</strong> hydrate <strong>of</strong> llme, or'that form producedby slaking freshly burned or'quick lime With water. Its caustic property iJgreatest directly after being slaked: Figaro that time <strong>the</strong> carbonic aeld <strong>of</strong> <strong>the</strong> at*mosphere, uniting with it_ drives <strong>of</strong>f <strong>the</strong> water, and taking its place diminishesitseaustloproperty.TMs actioncontinuesunt!lallt_e waterisdriven<strong>of</strong>l_anditbecomescarbonate<strong>of</strong>llme,or mildlime.NEW JERSEY GEOLOGICAL SURVEY

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