浅议土地储备制度存在的问题及对策

一、我国土地储备制度的产生是历史发展的必然 据2003年统计，我国国有资产总量为33万亿元，其中国有土地资产就有25万亿元，约占80%。在计划经济体制下，这笔巨额土地资产隐含在土地的无偿、无限期、无流动使用之中。随着社会主义市场经济体制的不断深入和完善，如何加快土地制度改革步伐，将巨额土地资产尽快显化、盘活并作为一种资本经营，对于推动经济发展，推进城市化进程具有重要的战略性意义。     

京都议定书带来商机 国际争购中国减排额

日前,旨在减缓全球气候变化的《京都议定书》正式生效一年,随着议定书中核心内容清洁机制在中国市场的建立,外国投资者纷纷来到中国购买“减排额”。据有关方面人士估计,未来全球一半的清洁发展机制市场将在中国。据国际非盈利环保组织绿色和平介绍,目前全球碳市场已经形成,二氧化碳排放成为一种新的商品在国际资本市场流通,各     

论中国商业经济区的划分

自改革开放以来,我国的商品经济发展很快。已由原来的单一计划经济,进入有计划的商品经济这一历史发展时期。商品的流通已成为促进区域商品生产、满足市场消费、加强区域经济联系的桥梁和纽带。因此,在劳动地域分工的基础上,研究和划分按商品流通的客观规律自然形成的商业经济地理区域;是地理科学,特别是人文地理学所面临的一项迫切任务。地域是商品经济活动的载体,科学地划分不同层次商品经济区域,它对于发展生产、繁荣经济、形成全国统一的市场、进入世界经济大循环具有重要的现实意义。     

VERTICAL PROFII,ES OF CHL-A AND PRIMARY PRODUCTIVITY IN THE MIDDLE CONTINENTAL SHELF AREA AND EDDY AREA OF THE EAST CHINA SEA

Vertical profiles of chl-a and primary productivity in the middle continental shelf area and eddy area of the East China Sea were studied using data from a cruise in the East China Sea in February to March, 1997 and a cruise in July, 1998. The results showed that chl-a vertical distribution closely related to in situ hydrological and nutrient conditions. Chla-a concentration ranged from 0.22 to 0.35 mg/m³ and 0.93–1.09 mg/m³ in the eddy area and in the middle continental shelf area, respectively. In both areas, chl-a concentrations in deep layers were slightly higher than those in shallow layers, but was of the same order of magnitude. In summer, when a thermocline existed in the water column, highest chl-a concentrations appeared at the base of the thermocline layers in both areas. In the eddy area, chl-a concentration maximized at 31.743 mg/m³, and averaged 1.143 mg/m³ below 30 m depth. In the middle continental shelf area, the highest chl-a concentration was 2.120 mg/m³, the average was 1.168 mg/m³. The primary productivity reached 1418.76 mgC/(m²·d) in summer and 1360.69 mgC/(m²·d) in winter. In the eddy area, the primary productivity was 787.50 mgC/(m²·d) in summer and 159.04 mgC/(m²·d) in winter. Vertical carbon sinking rate from the deep layer to the bottom in both areas is also discussed in this paper. Contribution NO. 4183 from the Institute of Oceanology, Chinese Academy of Sciences. Project No. 49636210 supported by NSFC.