I. Market Failure Market Power Externalities Public Goods Incomplete Information II. Rent Seeking III. Government Policy and International Markets

I. Basic Pricing Strategies Monopoly & Monopolistic Competition Cournot Oligopoly II. Extracting Consumer Surplus Price Discrimination  Two-Part Pricing Block Pricing  Commodity Bundling III. Pricing for Special Cost and Demand Structures

I. Conditions for Oligopoly? II. Role of Strategic Interdependence III. Profit Maximization in Four Oligopoly Settings Sweezy (Kinked-Demand) Model Cournot Model Stackelberg Model Bertrand Model

I. Market Structure Measures of Industry Concentration II. Conduct Pricing Behavior Integration and Merger Activity III. Performance Dansby-Willig Index Structure-Conduct-Performance Paradigm IV. Preview of Coming Attractions

I. Production Analysis Total Product, Marginal Product, Average Product Isoquants Isocosts Cost Minimization II. Cost Analysis

I. Elasticities of Demand Own Price Elasticity Elasticity and Total Revenue Cross-Price Elasticity Income Elasticity II. Demand Functions

Overview I. Introduction II. The Economics of Effective Management Identify Goals and Constraints Recognize the Role of Profits Understand Incentives Understand Markets Recognize the Time Value of Money Use Marginal Analysis

一、岩溶作用 地下水和地表水对可溶性岩石的破坏和再 造作用，包括化学作用过程（溶解和沉淀）和 物理作用过程（流水的侵蚀和堆积、重力的塌 陷和堆积），但化学作用过程是塑造喀斯特地 貌的主要动力

 海岸是具有一定宽度的陆地与海洋相互作用的地带。  可划分为滨海陆地、海滩和水下岸坡。  滨海陆地是高潮线以上至风暴浪所能作用的区域  海滩是高潮位和低潮位之间的地带  水下岸坡是底潮线以下到海浪作用开始掀起海底泥沙处

一、地下水的物理性质和化学成分 （一）地下水的物理性质 1.温度 地下水的温度是因自然条件不同而变化 的。极地、高纬和山区的地下水温度很低、地 壳深处和火山活动区的地下水温度很高。地下 水温度通常与当地气温有一定的关系，温带和 亚热带平原区的浅层地下水，年平均温度比所 在地区年平均气温高1—2℃