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International Demand (international + demand)
Selected AbstractsExploring strategic priorities for regional agricultural R&D investments in East and Central AfricaAGRICULTURAL ECONOMICS, Issue 2 2010Liangzhi You O13; O32; O55; Q16 Abstract The 11 countries of East and Central Africa have diverse but overlapping agroclimatic conditions, and could potentially benefit from spillovers of agricultural technology across country borders. This article uses high-resolution spatial data on actual and potential yields for 15 major products across 12 development domains to estimate the total benefits available from the spread of new agricultural technologies around the region. Market responses and welfare gains are estimated using the,Dynamic Research Evaluation for Management,model, taking account of current and future projections of local and international demand. Results suggest which crops, countries, and agroclimatic regions offer the largest total benefits. Downloadable data and program files permit different assumptions and additional information to be considered in the ongoing process of strategic priority setting. [source] Sustainability of the dimension stone industry in Zimbabwe,challenges and opportunitiesNATURAL RESOURCES FORUM, Issue 3 2001Oliver Maponga Abstract The rapid expansion of the dimension stone and black granite industry in Zimbabwe in the 1990s, a result of increasing domestic and international demand for black granite, has ushered in new challenges and opportunities for producers and beneficiaries alike. This article investigates the social, environmental and economic challenges emanating from the export boom, the economic opportunities presented by the expanding market and the potential role the robust industry could play in regional economic development and poverty alleviation. The article evaluates the long-term sustainability of the dimension stone industry and recommends the reinvestment of revenues into diversification of the regional economic base, upgrading of local infrastructure, further processing of rough stone before export and encouragement of micro-businesses to enhance sustainability. The author argues for modification of economic incentives to incorporate environmental and social objectives in order to enhance sustainability. The need for a holistic approach to policies affecting the exploitation, processing and marketing of granite resources and their products is recognized. More research on the operations of the industry is called for. [source] Rare Earth Deposits of North AmericaRESOURCE GEOLOGY, Issue 4 2008Stephen B. Castor Abstract Rare earth elements (REE) have been mined in North America since 1885, when placer monazite was produced in the southeast USA. Since the 1960s, however, most North American REE have come from a carbonatite deposit at Mountain Pass, California, and most of the world's REE came from this source between 1965 and 1995. After 1998, Mountain Pass REE sales declined substantially due to competition from China and to environmental constraints. REE are presently not mined at Mountain Pass, and shipments were made from stockpiles in recent years. Chevron Mining, however, restarted extraction of selected REE at Mountain Pass in 2007. In 1987, Mountain Pass reserves were calculated at 29 Mt of ore with 8.9% rare earth oxide based on a 5% cut-off grade. Current reserves are in excess of 20 Mt at similar grade. The ore mineral is bastnasite, and the ore has high light REE/heavy REE (LREE/HREE). The carbonatite is a moderately dipping, tabular 1.4-Ga intrusive body associated with ultrapotassic alkaline plutons of similar age. The chemistry and ultrapotassic alkaline association of the Mountain Pass deposit suggest a different source than that of most other carbonatites. Elsewhere in the western USA, carbonatites have been proposed as possible REE sources. Large but low-grade LREE resources are in carbonatite in Colorado and Wyoming. Carbonatite complexes in Canada contain only minor REE resources. Other types of hard-rock REE deposits in the USA include small iron-REE deposits in Missouri and New York, and vein deposits in Idaho. Phosphorite and fluorite deposits in the USA also contain minor REE resources. The most recently discovered REE deposit in North America is the Hoidas Lake vein deposit, Saskatchewan, a small but incompletely evaluated resource. Neogene North American placer monazite resources, both marine and continental, are small or in environmentally sensitive areas, and thus unlikely to be mined. Paleoplacer deposits also contain minor resources. Possible future uranium mining of Precambrian conglomerates in the Elliott Lake,Blind River district, Canada, could yield by-product HREE and Y. REE deposits occur in peralkaline syenitic and granitic rocks in several places in North America. These deposits are typically enriched in HREE, Y, and Zr. Some also have associated Be, Nb, and Ta. The largest such deposits are at Thor Lake and Strange Lake in Canada. A eudialyte syenite deposit at Pajarito Mountain in New Mexico is also probably large, but of lower grade. Similar deposits occur at Kipawa Lake and Lackner Lake in Canada. Future uses of some REE commodities are expected to increase, and growth is likely for REE in new technologies. World reserves, however, are probably sufficient to meet international demand for most REE commodities well into the 21st century. Recent experience shows that Chinese producers are capable of large amounts of REE production, keeping prices low. Most refined REE prices are now at approximately 50% of the 1980s price levels, but there has been recent upward price movement for some REE compounds following Chinese restriction of exports. Because of its grade, size, and relatively simple metallurgy, the Mountain Pass deposit remains North America's best source of LREE. The future of REE production at Mountain Pass is mostly dependent on REE price levels and on domestic REE marketing potential. The development of new REE deposits in North America is unlikely in the near future. Undeveloped deposits with the most potential are probably large, low-grade deposits in peralkaline igneous rocks. Competition with established Chinese HREE and Y sources and a developing Australian deposit will be a factor. [source] Designing the Gastronomic QuarterARCHITECTURAL DESIGN, Issue 3 2005Susan Parham Abstract Throughout the world, urban gastronomic quarters, centred on fresh-food markets, have been pulled back from the brink of extinction. Susan Parham explains how movements like Slow Food and Slow Cities in Italy, and the international demand for organic produce, have started to challenge the global food network of production and consumption. The growing revitalisation of urban quarters around produce markets not only serves customers seeking fresh produce, food products and lively cafés and restaurants, but also offers valuable lessons in urban design. [source] |