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

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

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 动物消化饲料的方式 第二节 消化后养分的吸收 第三节 动物的消化力与饲料的可消化性 一、消化力与消化性 二、影响消化率的因素

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

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

盐渍土是重要的土地资源，土壤盐渍化是影响农业生产和园林建设的关键因素。本研究在崇明东滩北部农场区的10个样区中布置了33个样点，共采集了89个土壤样品，进行了土壤主要理化性质及盐碱性的测试和统计分析

Plant K A. Potassium content of plants 1.20-50gkg-1 2. Plants take up large amount of K. Only N is taken up more. 3. In some plants (sugar beets and potatoes) K uptake is greater than N uptake

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