期刊文献+

浙江中部红壤施用石灰对土壤交换性钙、镁及土壤酸度的影响 被引量:114

EFFECT OF LIMING ON ACIDITY AND EXCHANGEABLECALCIUM AND MAGENSIUM OF RED SOILIN CENTRAL ZHEJIANG
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摘要 为了确定红壤施用石灰后钙、镁移动和土壤酸化速率,监测了耕层(10~20cm)和底土(20~60cm)的pH和交换性Ca2+、Mg2+、Al3+的长期变化。结果表明,耕层交换性Ca2+在施用石灰后的一年半时间达到最高值,此后随着时间的推移而急剧减少;而底土的交换性Ca2+随石灰用量的增加和施用石灰后时间的推移而增加。镁在土壤剖面中的移动比钙快;施用石灰后耕层和底土酸度的降低与交换性Ca2+的增加基本同步。在本试验条件下,不论施用石灰与否都存在着复酸化过程,但施用石灰后复酸化作用更强。 A 14year experiment consisted of five treatments (0,3750,7500,11250, and 15000 kg ground limestone/hm2) started in July 1980 on a virgin red soil derived from Quaternary red clay which had a initial pH of 4.86 and exchangeable A1 of 5.46 cmol(+)/kg. To determine movement of Ca and Mg in the soil profiles and quantify acidification rates of the limeamended soil, changes of soil pH and exchangeable Ca, Mg, and A1 in plough layer (020cm) and subsoil (2060 cm) of the soils receiving different amounts of lime were monitored. The levels of exchangeable Ca in plough layers of the limed treatments reached the maxima 1.5 years after liming and sharply declined ever since. The changes of soil acidity in plough layers turned out contrary to the changes of exchangeable Ca. Ca movement and the depth of neutralization increased with increasing lime rate and time after liming. Acidity neutralization in subsoils as measured by decreased in exchangeable A1 and increased in soil pH was more obvious 4 years after liming. Decline in soil acidity in subsoil increased with increasing lime rates and time after liming. Magnesium movement was faster than Ca movement in the soil profiles. Acidification rates of nonlimed treatment were pH 0.02 unit and exchangeable Ca 0.06 cmol(+)/kg per year, while those of limed treatments were pH 0.190.20 unit, and exchangeable Ca 0.380.21 cmol (+)/kg per year. The residue effect of the treatment receiving recommended lime rate (7500 ground limestone kg/hm2) could last 15 years. Overliming (15000 kg ground limestone/hm2) did not result in decrease in crop yields because the depth of neutralization in subsoil acidity of the treatment was greater than those for the treatments receiving lower lime rates.
出处 《植物营养与肥料学报》 CAS CSCD 1999年第2期129-136,共8页 Journal of Plant Nutrition and Fertilizers
基金 浙江省自然科学基金
关键词 红壤 石灰 移动 土壤酸度 Red soil LimingMovement of calcium and nagnesiumSoil acidityReacidification
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参考文献6

  • 1孟赐福,傅庆林,水建国,周梅芳.土壤酸度对大豆、油菜生长和产量的影响[J].中国农业科学,1994,27(3):63-70. 被引量:22
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二级参考文献7

  • 1曹一平,高等植物的矿质营养,1991年
  • 2孟赐福,中国油料,1988年,2期,45页
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  • 7刘勋,江西红壤研究.2

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