• Applied Biological Chemistry
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• v.29 no.2
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• pp.107-115
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• 1986

The chemical changes and the quality of the soysauce which was Bade by new convenient method using vinyl teat instead of koji room, replacing wheat with milled barley koji were investigated. Protease activity of the koji was higher as tile ratio of soybeans was increased but amylase activity was higher as the ratio of milled barley was increased. The amounts of total nitrogen showed substantial increases until 80 days and afterwards, their rates of increases were lower. The more its content of soybeans, the higher its amount of total nitrogen, The amount of amino nitrogen increased slowly in all samples and the sample which had a large amount of soybeans was higher than those with small amounts of soybeans. The amount of ammonia nitrogen showed increases until 120 days tut decreased after then. The amount of reducing sugar showed increases until 80 days and decreased after then and the greater its source of carton, the higher its amount of reducing sugar. The total acid contort had large increases until 100 days in all samples and afterward they did not show any particular changes. The changes of pH decreased for 100 days and afterwards, they increased a little. In the original soysauce, combined ratio of soybean 3 to milled barley 2 and the sample of those ratio 4 : 1 are better than others and in diluted soysauce combined ratio of soybean 4 to milled barley 1 is better than the others. In original soysauce the use of $20{\sim}40%$ barley koji, which is added to soybeans, is superior and diluted soysauce the use of 20% barley koji is superior.

• Journal of the Korean earth science society
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• v.18 no.6
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• pp.500-514
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• 1997

With respect to the amphibolites in the Mungyong area of the central part of the Ogcheon Fold Belt, detail field occurrence, texture and geochemical properties within each sills and petrogenetic environment are presented. We confirmed that the amphibolites in the Sangnaeri Formation (Ogcheon Supergroup) and limestone(Cambro-Ordovician Chosun Supergroup) sequences are metamorphosed dolerite sills which are roughly concordant to bedding of country rocks. Geologic distribution of the rocks is distinctly improved compared with those of previous investigations. There are four main sills so far observed in the study area. One is emplaced in limestone(Ls Sill, about 3 m thick) and the others are emplaced in Sangnaeri Formation, which are named First Sill(about 40 m thick), Second Sill(about 100 m thick) and Third Sill(about 40 m thick) from lower to upper horizons of the meta-pelitic sequences. The thick sills are intruded by minor sills and the Third Sill is a composite sill consisting of two main and two minor sills. Each sill has fine grained chilled marginal zones and grain size increases inwards from both contacts. The Second Sill has various vein and white patch in central part and the rock compositions vary systematically from margin to central part. $SiO_2,\;Na_2O,\;K_2O\;and\;P_2O_5$ increase, whereas $TiO_2,\;FeO,\;Al_2O_3\;and\;CaO$ decrease toward the contort. We investigate the major and trace element variations of ten selected rock compositions as intruding initial magma take occurrence and chemical properties into consideration. The compositional variations of them can not be explained by fractionation crystallization of single magma. Geologic distribution, geochemical properties and previous data suggest that amphibolite precursors(basaltic magma) of the study area were intrusive as sill-like in an intracontinental rift environment.