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Influence of form, soil-zone, and fineness of lime and magnesia incorporations upon outgo of calcium and magnesium

被引：9
作者：
MacIntire, WH
机构：
来源：
SOIL SCIENCE | 1926年 / 21卷 / 05期
关键词：
D O I：
10.1097/00010694-192605000-00003
中图分类号：
S15 [土壤学];
学科分类号：
0903 ; 090301 ;
摘要：
引用
收藏
页码：377 / 391
页数：15
相关论文
共 5 条
[1]   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
[2]   Sulfur, calcium, magnesium and potassium content and reaction of rainfall at different points in Tennessee [J].
MacIntire, WH ;
Young, JB .
SOIL SCIENCE, 1923, 15 (03) :205-227
[3]   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
[4]  
MACINTIRE WH, 1923, SOIL SCI, V16, P121
[5]  
MACINTIRE WH, 1919, SOIL SCI, V7, P351
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