Fixation of calcium-magnesium from burnt limes, limestone and dolomite incorporations in two soil zones

被引：5

作者：

MacIntire, WH

Shaw, WM

机构：

来源：

SOIL SCIENCE | 1926年 / 22卷 / 02期

关键词：

D O I：

10.1097/00010694-192608000-00003

中图分类号：

S15 [土壤学];

学科分类号：

0903 ; 090301 ;

摘要：

引用

页码：109 / 121

页数：13

共 14 条

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[2]

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[3]

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[4]

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[5] The role of silica in counteracting magnesia-induced toxicity [J].

MacIntire, WH ;

Shaw, WM ;

Young, JB .

SOIL SCIENCE, 1925, 19 (05) :331-341

[6] Reciprocal repression exerted by calcic and magnesic additions upon the solubility of native materials in surface soil [J].

MacIntire, WH ;

Shaw, WM ;

Young, JB .

SOIL SCIENCE, 1923, 16 (06) :449-464

[7] Influence of form, soil-zone and fineness of lime and magnesia incorporations upon outgo of sulfates and nitrates [J].

MacIntire, WH .

SOIL SCIENCE, 1926, 22 (01) :21-30

[8] Influence of form, soil-zone, and fineness of lime and magnesia incorporations upon outgo of calcium and magnesium [J].

MacIntire, WH .

SOIL SCIENCE, 1926, 21 (05) :377-391

[9] The disintegration of limestone and dolomite separates as influenced by zone of incorporation [J].

MacIntire, WH ;

Shaw, WM .

SOIL SCIENCE, 1925, 20 (05) :403-417

[10]

MACINTIRE WH, 1925, SOIL SCI, V19, P126

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