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

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84On "examination and comparison <strong>of</strong> <strong>the</strong> results <strong>of</strong> <strong>the</strong>se'twoanalyses, several considerations present <strong>the</strong>mselves. In <strong>the</strong>first place_ <strong>the</strong> presence <strong>of</strong> soluble salts <strong>of</strong> lime is an unexpectedresult. It is unfortunate that time has n6t yet alloweddeterminations to be made <strong>of</strong> <strong>the</strong> quantit!es <strong>of</strong> <strong>the</strong>se solublesalts which are present, but <strong>the</strong>ir pretence at all in appreciablefluautity is <strong>of</strong> much practical importance. It is in <strong>the</strong> form <strong>of</strong>soluble salts only, that lime can act directly ms an aliment <strong>of</strong>plants, that is, in this form only can it be takhn up by. <strong>the</strong>irrootlets. ]i'arthcr investigation will probably indicate practicablemeans <strong>of</strong> increasing <strong>the</strong> production <strong>of</strong> <strong>the</strong>se solublesalts, and <strong>of</strong> thus greatly'augmenting <strong>the</strong> vah_e <strong>of</strong> such marlsas fertilizers.. Lime, however, is not <strong>the</strong> only ingredient -<strong>of</strong> importanceindicated by <strong>the</strong> analyses. Nearly every o<strong>the</strong>r substancefound to be present has more or less influence. 'The magnesia,oxide <strong>of</strong> iron, phosphate <strong>of</strong> lime, and amorphous silica arc allabsolutely necessary constituents <strong>of</strong> all fertile soils_ while <strong>the</strong>organic acids, and o<strong>the</strong>r products <strong>of</strong> vcgctab_b decay, whichappear to be preseflt in quite important quantity (six or sevenper cent.), also contribute ihdirectly <strong>the</strong>ir influence. T!lc organicacids i esp6cia]Iy_ undoubtedly: act by forming compoundsWith lime, and o<strong>the</strong>r bases present, which are soluble ill <strong>the</strong>liquids <strong>of</strong> <strong>the</strong> soil, thus ncccssitating thcirintroduetion into <strong>the</strong>circulation <strong>of</strong> plants by <strong>the</strong> cndosmotie absorption <strong>of</strong> <strong>the</strong> roots ;and if <strong>the</strong> now mooted question, wMeh will p_'obably receivesome discussion in ftlturc reports, whe<strong>the</strong>r <strong>the</strong> nitrogen <strong>of</strong>vegetable tissues be derived from ammonia or hot_ admits <strong>of</strong> anaffirmative dccision_ <strong>the</strong> organic acids must also act indircetly_though powerfully, by retaining <strong>the</strong> ammoniaproduced during<strong>the</strong> dcc_y <strong>of</strong> <strong>the</strong> animal matter <strong>of</strong> <strong>the</strong> shells, in a highly solubleform, and also by absorbing atmospheric.ammonia, or even,as indicated by" Muldcr,* through <strong>the</strong> development <strong>of</strong> .ammoniaby <strong>the</strong> cgmbination <strong>of</strong> <strong>the</strong> nitrogen o:f <strong>the</strong> air with <strong>the</strong>hydrogen produced by <strong>the</strong>ir own deeomp0sigon. It will be* As quoted in Loewig's "Chemic der Organischon Vorbindungen," i,, 474;NEW JERSEY GEOLOGICAL SURVEY

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