7.1 土壤的酸性和碱性反应 7.2 土壤酸碱性的指标 7.3 土壤的缓冲性 7.4 土壤氧化还原反应

第一节 粘土矿物 第二节 土壤胶体 第三节 土壤胶体的表面性质 第四节 土壤胶体对阳离子的吸附交换反应 第五节 土壤胶体对阴离子的吸附与交换

第一节 土壤水的类型划分土壤水含量 第二节 土壤水的能态 第三节 土壤水的运动 第四节 土壤空气状况 第五节 土壤热量状况

Acknowledge I expresses thanks to Assoc. Prof. rob Reid of Adelaide university of Australia, Dr Jeff Gale, foreign teacher of northwest A&F University of China, and Prof. Zhang Fusuo, Prof. Li Xiaolin of China Agriculture University, Prof Liu Yuanyin of Northeast agriculture Unversity and other authors who provide materials for me, or whose materials, such as photographs and figures etc, I used in the lectures

有机质的来源和组成 土壤有机物质的分解和转化 土壤腐殖物质的形成和性质 土壤有机质的作用及管理

第一节 复合肥料的意义和发展动向 第二节 复合肥料的种类和施用 第三节 肥料的配比和混合

Phosphorus in plant physiology P content of plants Approximately 0.2% of plant dry weight is P Plants require a relatively large amount of P. The phosphate concentration in the cytosol is maintained at fairly constant concentrations in the 5 to 8 mol/m3 regardless of the external phosphate concentration except under severe P deficiency. By contrast is the vacuolar phosphate concentration

Plant nitrogen 1.1 Uptake of N 1. N is required by plants in large amounts Most plant material contains 2-4%N and 40%C. 2. N is usually the limiting nutrient in unfertilized systems 3. Most n is taken up from the soil in the form of nht or no a small amount of NH3 can be absorbed through the leaves N2 can be used by legume plant via biological nitrogen fiXation

肥料的定义与包容 肥料在农业生产中的作用 现代农业中肥料的应用状况 当今肥料应用方面所面临的问题 肥料学的目的与任务

Calcium in physiology Uptake and translocation Higher plants often contain apprecia ble amounts Ca and generally in the order of about 5-30 mg Ca/g dry matter The high Ca2+ concentrations related with the high Ca2+ levels in media not related with the Ca2+ uptake