Nd, Sr and Pb isotopic composition of eolian dust deposited in the central North Pacific

The silicate fractions of recent pelagic sediments in the central north Pacific Ocean are dominated by eolian dust derived from central Asia. An 11 Myr sedimentary record at ODP Sites 885/886 at 44.7°N, 168.3°W allows the evaluation of how such dust and its sources have changed in response to late Cenozoic climate and tectonics. The extracted eolian fraction contains variable amounts (>70%) of clay minerals with subordinate quartz and plagioclase. Uniform Nd isotopic compositions (epsilon-Nd =38.6 to 310.5) and Sm/Nd ratios (0.170-0.192) for most of the 11 Myr record demonstrate a well-mixed provenance in the basins north of the Tibetan Plateau and the Gobi Desert that was a source of dust long before the oldest preserved Asian loess formed. epsilon-Nd values of up to 36.5 for samples 62.9 Ma indicate <=35 wt% admixture of a young, Kamchatka-like volcanic arc component. The coherence of Pb and Nd in the erosional cycle allows us to constrain the Pb isotopic composition of Asian loess devoid of anthropogenic contamination to 206Pb/204Pb =18.97 +/- 0.06, 207Pb/204Pb =15.67 +/- 0.02, 208Pb/204Pb =39.19 +/- 0.11. 87Sr/86Sr (0.711-0.721) and Rb/Sr ratios (0.39-1.1) vary with dust mineralogy and provide an age indication of ~250 Ma. 40Ar/39Ar ages of six dust samples are uniform around 200 Ma and match the K-Ar ages of modern dust deposited on Hawaii. These data reflect the weighted age average of illite formation. Changes from illite- smectite with significant kaolinite to illite- and chlorite-rich, kaolinite-free assemblages since the late Pliocene document changes in the intensity of chemical weathering in the source region. Such weathering evidently did not disturb the K-Ar systematics, and only induced scatter in the Rb-Sr data. We propose that when smectite forms at the expense of illite, K and Ar are quantitatively lost from what becomes smectite, but are quantitatively retained in adjacent illite layers. 40Ar/39Ar age data, therefore, are insensitive to smectite formation during chemical weathering but date the diagenetic growth of illite, the major K-bearing phase in the dust. Over the past 12 Myr, the dust flux to the north Pacific increased by more than an order of magnitude, documenting a substantial drying of central Asia. This climatic change, however, did not alter the ultimate source of the dust, and neoformational products of chemical weathering always remained subordinate to assemblages reworked by mechanical erosion in dust deposited in eastern Asia and the Pacific Ocean.

Concentrations and accumulation rates of chemical elements and sediment components in sediments of central equatorial Pacific, DSDP data

Accumulation rates of Mg, Al, Si, Mn, Fe, Ni, Cu, Zn, opal, and calcium carbonate have been calculated from their concentrations in samples from equatorial Deep Sea Drilling Project sites. Maps of element accumulation rates and of Q-mode factors derived from raw data indicate that the flux of trace metals to equatorial Pacific sediments has varied markedly through time and space in response to changes in the relative and absolute influence of several depositional influences: biogenic, detrital, authigenic, and hydrothermal sedimentation. Biologically derived material dominates the sediment of the equatorial Pacific. The distributions of Cu and Zn are most influenced by surface-water biological activity, but Ni, Al, Fe, and Mn are also incorporated into biological material. All of these elements have equatorial accumulation maxima similar to those of opal and calcium carbonate at times during the past 50 m.y. Detritus distributed by trade winds and equatorial surface circulation contributes Al, non-biogenic Si, Fe, and Mg to the region. Detrital sediment is most important in areas with a small supply of biogenic debris and low bulk-accumulation rates. Al accumulation generally increases toward the north and east, indicating its continental source and distribution by the northeast trade winds. Maxima in biological productivity during middle Eocene and latest Miocene to early Pliocene time and concomitant well-developed surface circulation contributed toward temporal maxima in the accumulation rates of Cu, Zn, Ni, and Al in sediments of those ages. Authigenic material is also important only where bulk-sediment accumulation rates are low. Ni, Cu, Zn, and sometimes Mn are associated with this sediment. Fe is almost entirely of hydrothermal origin. Mn is primarily hydrothermal, but some is probably scavenged from sea water by amorphous iron hydroxide floes along with other elements concentrated in hydrothermal sediments, Ni, Cu, and Zn. During the past 50 m.y. all of these elements accumulated over the East Pacific Rise at rates nearly an order of magnitude higher than those at non-rise-crest sites. In addition, factor analysis indicates that some of this material is carried substantial distances to the west of the rise crest. Accumulation rates of Fe in basal metalliferous sediments indicate that the hydrothermal activity that supplied amorphous Fe oxides to the East Pacific Rise areas was most intense during middle Eocene and late Miocene to early Pliocene time.

Database of Ice-Rich Yedoma Permafrost (IRYP)

Vast portions of Arctic and sub-Arctic Siberia, Alaska and the Yukon Territory are covered by ice-rich silty to sandy deposits that are containing large ice wedges, resulting from syngenetic sedimentation and freezing. Accompanied by wedge-ice growth in polygonal landscapes, the sedimentation process was driven by cold continental climatic and environmental conditions in unglaciated regions during the late Pleistocene, inducing the accumulation of the unique Yedoma deposits up to >50 meters thick. Because of fast incorporation of organic material into syngenetic permafrost during its formation, Yedoma deposits include well-preserved organic matter. Ice-rich deposits like Yedoma are especially prone to degradation triggered by climate changes or human activity. When Yedoma deposits degrade, large amounts of sequestered organic carbon as well as other nutrients are released and become part of active biogeochemical cycling. This could be of global significance for future climate warming as increased permafrost thaw is likely to lead to a positive feedback through enhanced greenhouse gas fluxes. Therefore, a detailed assessment of the current Yedoma deposit coverage and its volume is of importance to estimate its potential response to future climate changes. We synthesized the map of the coverage and thickness estimation, which will provide critical data needed for further research. In particular, this preliminary Yedoma map is a great step forward to understand the spatial heterogeneity of Yedoma deposits and its regional coverage. There will be further applications in the context of reconstructing paleo-environmental dynamics and past ecosystems like the mammoth-steppe-tundra, or ground ice distribution including future thermokarst vulnerability. Moreover, the map will be a crucial improvement of the data basis needed to refine the present-day Yedoma permafrost organic carbon inventory, which is assumed to be between 83±12 (Strauss et al., 2013, doi:10.1002/2013GL058088) and 129±30 (Walter Anthony et al., 2014, doi:10.1038/nature13560) gigatonnes (Gt) of organic carbon in perennially-frozen archives. Hence, here we synthesize data on the circum-Arctic and sub-Arctic distribution and thickness of Yedoma for compiling a preliminary circum-polar Yedoma map. For compiling this map, we used (1) maps of the previous Yedoma coverage estimates, (2) included the digitized areas from Grosse et al. (2013) as well as extracted areas of potential Yedoma distribution from additional surface geological and Quaternary geological maps (1.: 1:500,000: Q-51-V,G; P-51-A,B; P-52-A,B; Q-52-V,G; P-52-V,G; Q-51-A,B; R-51-V,G; R-52-V,G; R-52-A,B; 2.: 1:1,000,000: P-50-51; P-52-53; P-58-59; Q-42-43; Q-44-45; Q-50-51; Q-52-53; Q-54-55; Q-56-57; Q-58-59; Q-60-1; R-(40)-42; R-43-(45); R-(45)-47; R-48-(50); R-51; R-53-(55); R-(55)-57; R-58-(60); S-44-46; S-47-49; S-50-52; S-53-55; 3.: 1:2,500,000: Quaternary map of the territory of Russian Federation, 4.: Alaska Permafrost Map). The digitalization was done using GIS techniques (ArcGIS) and vectorization of raster Images (Adobe Photoshop and Illustrator). Data on Yedoma thickness are obtained from boreholes and exposures reported in the scientific literature. The map and database are still preliminary and will have to undergo a technical and scientific vetting and review process. In their current form, we included a range of attributes for Yedoma area polygons based on lithological and stratigraphical information from the original source maps as well as a confidence level for our classification of an area as Yedoma (3 stages: confirmed, likely, or uncertain). In its current version, our database includes more than 365 boreholes and exposures and more than 2000 digitized Yedoma areas. We expect that the database will continue to grow. In this preliminary stage, we estimate the Northern Hemisphere Yedoma deposit area to cover approximately 625,000 km². We estimate that 53% of the total Yedoma area today is located in the tundra zone, 47% in the taiga zone. Separated from west to east, 29% of the Yedoma area is found in North America and 71 % in North Asia. The latter include 9% in West Siberia, 11% in Central Siberia, 44% in East Siberia and 7% in Far East Russia. Adding the recent maximum Yedoma region (including all Yedoma uplands, thermokarst lakes and basins, and river valleys) of 1.4 million km² (Strauss et al., 2013, doi:10.1002/2013GL058088) and postulating that Yedoma occupied up to 80% of the adjacent formerly exposed and now flooded Beringia shelves (1.9 million km², down to 125 m below modern sea level, between 105°E - 128°W and >68°N), we assume that the Last Glacial Maximum Yedoma region likely covered more than 3 million km² of Beringia. Acknowledgements: This project is part of the Action Group "The Yedoma Region: A Synthesis of Circum-Arctic Distribution and Thickness" (funded by the International Permafrost Association (IPA) to J. Strauss) and is embedded into the Permafrost Carbon Network (working group Yedoma Carbon Stocks). We acknowledge the support by the European Research Council (Starting Grant #338335), the German Federal Ministry of Education and Research (Grant 01DM12011 and "CarboPerm" (03G0836A)), the Initiative and Networking Fund of the Helmholtz Association (#ERC-0013) and the German Federal Environment Agency (UBA, project UFOPLAN FKZ 3712 41 106).

Animation with all MODIS fire product maps from 2000 to 2011, Yakutia, Siberia

The video FireMovie_2000-2011.avi shows an animation with all MODIS fire product maps of the area sequenced over time. Colors in the video describe MODIS classes as follows: MODIS classification and color scale: Class 0 - not processed - Dark blue (1 frame) Class 3 - water - Light Blue (rivers and some lakes) Class 4 - clouds - Green blue Class 5 - non fire land - Yellow green Class 8 - nominal confidence fire - Red Class 9 - high confidence fire - Dark red

Financial Cooperation in East Asia

This paper addresses the rationale for financial cooperation in East Asia. It begins by giving a brief review of developments after the Asian currency crisis, and argues that enhancing regional financial cooperation both quantitatively and qualitatively will require: (1) upgrading surveillance capabilities in the region, and (2) creating a clear division of labor between regional institutions and the IMF. It also mentions the issue of membership and the background forces that have led to the duplication of similar forums in East Asia. Although the concern over crisis management is the central issue in East Asian financial cooperation, other issues such as exchange rate policy coordination and fostering regional capital markets are discussed as well.

Industrial Policy in Asia

This paper examines three types of industrialization that have occurred in East Asia: the Japanese, Chinese and generic Asian models. Industrial policies in Japan and the Republic of Korea (ROK) initially protected local companies from foreign investors by imposing high tariffs on foreign investors. But Japan began introducing liberalization policies to attract foreign direct investment (FDI) in the 1960s, and the ROK began to welcome foreign technology in the 1970s. Meanwhile, the governments of the ASEAN countries and Taiwan established export-processing zones (EPZ) to invite FDI by offering preferential treatment, such as tax deductions and exemptions. China adopted similar industrial policies and also established EPZs, attracting the capital and know-how of multinationals and thereby strengthening the international competitiveness of local enterprises. This paper reaches the following three conclusions. First, it would have been difficult for East Asian countries to grow without FDI. Second, central governments were a crucial factor in these countries' growth strategies. Third, EPZs offering preferential treatment can effectively enhance aggregate growth in developing countries, and the Asian experience shows that this strategy can be applied to other countries that satisfy certain preconditions.

Border Barriers in Agricultural Trade and the Impact of their Elimination: Evidence from East Asia

Abstract: By means of a GTAP based-CGE model, we investigate the impact of the elimination of import tariffs and non-tariff policy barriers (NTPBs) on agricultural trade towards East Asian FTAs. To do that, we first measure the NTPBs by employing a widely-used method derived from the literature on border effects. Next, by adding into the GTAP database our estimates on the NTPBs, which the original GTAP database by its nature does not succeed in incorporating, we compute the impact of the entire elimination of policy barriers (the complete reduction of import tariffs and of NTPBs) on GDP.

Commercialization of agriculture in the Himalayas

Increased market integration and commercialization of traditional agriculture in the Himalayas is part of a development strategy towards growth and better standard of living. More than 97 percent households depend upon agricultural and allied activities for livelihood which constitutes 30 percent of the household income. Given the importance of commercialization of agriculture to improve the productivity, per capita income and thereby the standard of living in the Himalayas, we examine the factors affecting the commercialization of agriculture on the basis of primary survey data. The results reveal that the land size, gender of the household head, livestock assets, ethnicity, education and location are important determinants of commercialization. Although commercialization of agriculture is considered as stimulated private-sector activity, public policy is essential to facilitate driving forces viz., trade and market reforms, rural infrastructure, and the institutional framework for legal and contractual arrangements between farmers and processors.

Chapter 7 Clusters of Modern and Local Industries in Vietnam

Since the introduction of the Doi Moi ('renovation') economic reform in 1986, Vietnam has experienced a transformation of its economic management, from a central planning economy to a market-oriented economy. High economic growth, created by the liberalization of activities in all sectors of the economy, has changed the economic structure of the country, and the once agriculture-based and poverty-stricken land now generates a midlevel income and possesses many industrial bases. Economic growth has also changed the landscape of the country. Business complexes have been built in metropolises like Ho Chi Minh City and Hanoi, and rice fields have been converted into industrial zones. As the number of enterprises increased, areas began to emerge where many enterprises agglomerated. Some of these 'clusters' were groups of cottage industry households, while many others were large-scale industrial clusters. As Porter [1998] argues, industrial clusters are the source of a nation's 'competitive advantage'. McCarty et al. [2005] indicate that in some key industries in Vietnam, some clusters of enterprises have been created, although the degree of agglomeration differs from one industry to another. Using industry census data from 2001, they include dot density maps for the 12 leading manufacturing industries in Vietnam. They show that most of the industries analyzed are clustered either in Hanoi or Ho Chi Minh City (or both). Among these 12 industries, the garments industry has the greatest tendency to cluster, followed by textile, rice, seafood, and paper industries. The fact that industrial clusters have begun to form in some areas could be a positive sign for Vietnam's future economic development. What is lacking in McCarty et al. [2005], however, is the identification of the participants in the industrial clusters. Some argue for the importance of small and medium enterprises (SMEs) in Vietnam's economic development (e.g. Nguyen Tri Thanh [2007], Tran Tien Cuong et al. [2008]), while others stress the impact of foreign direct investments (FDI) (for example, Tuan Bui [2009]). Adding information about the participants in the above cluster study (and in other studies of spatial patterns of location of enterprises) may broaden the scope for analysis of economic development in Vietnam. This study aims to reveal the characteristics of industrial clusters in terms of their participants and locations. The findings of the study may provide basic information for evaluating the effects of agglomeration and the robustness of the effects in the industrial clusters in Vietnam. Section 1 describes the characteristics of economic entities in Vietnam such as ownership, size of enterprise, and location. Section 2 examines qualitative aspects of industrial clusters identified in McCarty et al. [2005] and uses information on the size and ownership of clusters. Three key industries (garments, consumer electronics, and motor vehicle) are selected for the study. Section 3 identifies another type of cluster commonly seen in Vietnam, composed of local industries and called 'craft villages'. Many such villages have been developed since the early 1990s. The study points out that some of these villages have become industrialized (or are becoming industrialized) by introducing modern modes of production and by employing thousands of laborers.

Political economy of low sulfurization and air pollution control policy in Japan : SOx emission reduction by fuel conversion

In the early stages of the development of Japan’s environmental policy, sulfur oxide (SOx) emissions, which seriously damage health, was the most important air pollution problem. In the second half of the 1960s and the first half of the 1970s, the measures against SOx emissions progressed quickly, and these emissions were reduced drastically. The most important factor of the reduction was the conversion to a low-sulfur fuel for large-scale fuel users, such as the electric power industry. However, industries started conversion to low-sulfur fuel not due to environmental concerns, but simply to reduce costs. Furthermore, the interaction among the various interests of the electric power industry, oil refineries, the central government, local governments, and citizens over the energy and environmental policies led to the measures against SOx emissions by fuel conversion.

Agriculture Plus Plus : growth strategy for Myanmar agriculture

The development of agriculture is a main pillar of Myanmar’s growth strategies. It is natural for the Myanmar government to prioritize agriculture as a source of economic growth, since it accounted for 36% of GDP, employs a majority of labor force, and generates nearly 30% of exports as of 2010. Although the agricultural share in GDP and employment usually declines as an economy grows, it is not a sunset industry in Myanmar. Methods exist for increasing agriculture’s value added other than the growth of labor and land inputs. The key is to enhance three productivity measures: labor, land, and total productivity. We call this strategy "Agriculture Plus Plus."

The supply chain in East Asia

East Asia is a major tea-consuming and -producing area; however, few studies have examined the East Asian tea industry from the perspective of the supply chain. Based on field and desktop studies of the tea markets in Taiwan and China, this paper provides an overview of each market together with detailed case studies. In this analysis, the characteristics of the tea industry and the main problems in the current supply chain in terms of governance, upgrading, and food safety and quality control are identified. This paper will help fill the gap in studies of the East Asian tea industry from the perspective of the supply chain.

Provision of ecological infrastructures to increase pollinators and other beneficial organisms in rainfed crops in Central Spain

In sustainable intensive agriculture, the biodiversity of monoculture fields can be increased by managing the field margins to provide ecological infrastructures that serve as refuges and resources for beneficial organisms (pollinators and natural enemies). In the present work we summarize two years of field trials following the goal to increase biodiversity of beneficial fauna in a barley field in Central Spain by sowing different herbaceous mixtures in the field margins. The presence of arthropods visiting flowers on plots sown with different types of seed mixtures and unsown natural flora (control plot) was compared by visual sampling every week between April and June. The results showed that a combination of herbaceous big-size seeds was the most successful mixture emerging under our experimental conditions and achieved a higher number of visits of beneficial arthropods than the unsown natural vegetation.

Gestión de la fertilidad de suelos y la nutrición de plantaciones de teca (Tectona grandis L.f.) en América Central

La teca (Tectona grandis L.f.) ha sido tradicionalmente considerada como una madera preciosa en los países del SE Asiático, de donde es originaria, pero durante las últimas décadas ha alcanzado especial relevancia en el sector internacional de las maderas tropicales duras de buena calidad. La especie ha sido ampliamente establecida en América Central, donde tiene una gran importancia socioeconómica, tanto por el impacto de las grandes empresas multinacionales que gestionan grandes plantaciones en la región, como por el gran número de pequeños y medianos propietarios que han elegido esta especie para reforestar sus tierras. Pese a la gran importancia de esta especie, se ha desarrollado relativamente poca investigación acerca de su nutrición y de la gestión del suelo necesaria para su establecimiento y mantenimiento en condiciones sostenibles y productivas. En la presente Tesis Doctoral, tras realizar una amplia revisión bibliográfica, se caracterizan los suelos y la nutrición de las plantaciones de teca en América Central y se proponen varias herramientas para la mejora de su gestión. Las plantaciones de teca de América Central presentan habitualmente deficiencias de K y P, además de algunos problemas de acidez ocasionales. Estos se originan, principalmente, por la mala selección de sitio que se realizó en las últimas dos décadas del siglo XX y por el establecimiento de plantaciones de teca por pequeños propietarios en terrenos que no tienen características propicias para la especie. Además, estos problemas comunes relativos a la baja disponibilidad de P y de K en el suelo son causantes de las relativamente bajas concentraciones foliares de estos elementos (0,88±0,07% K y 0,16±0,04% P) encontradas en plantaciones de teca características de la región. Se presentan varios modelos estadísticos que permiten a los gestores: (a) usarlos como referencia para la interpretación de análisis foliares, ya que ofrecen valores que se consideran característicos de plantaciones de teca con un buen estado nutricional; (b) estimar la cantidad de nutrientes acumulados en la biomasa aérea de sus plantaciones y, sobre todo, su extracción a través de la madera en un aprovechamiento forestal, bien sea una clara o la corta final. La gran acumulación de N, P y K en plantaciones de teca ha de ser considerada como un factor fundamental en su gestión. Además, P y K adquieren mayor relevancia aún ya que su extracción del sistema a través de la madera y su escasa disponibilidad en los suelos hacen que se presente un importante desequilibrio que pone en riesgo la sostenibilidad del sistema. En ese sentido, cambiar la época de cosecha, de la actual (en Enero-Mayo) a Septiembre o Diciembre, puede reducir entre un 24 y un 28% la salida de N asociada a la extracción de madera, un 29% la de P y entre un 14 y un 43% la de K. Se estima que la concentración foliar de P es un factor limitante de la productividad de plantaciones de teca en América Central, proponiéndose un nivel crítico de 0,125%. Además, la teca presenta una tolerancia muy baja a suelos salinos, tendencia que no había sido señalada hasta el momento, siendo muy alta la probabilidad de que la plantación tenga un crecimiento lento o muy lento cuando la Saturación de Na es mayor de 1,1%. Por otro lado, se confirma que K es uno de los elementos clave en la nutrición de las plantaciones de teca en la región centroamericana, proponiéndose un nivel crítico provisional de 3,09% para la Saturación de K, por encima del cual es muy probable que la plantación tenga un crecimiento muy alto. Se ha comprobado que las técnicas estadísticas de análisis multivariante pueden ser usadas como herramientas para agrupar los rodales en base a sus similitudes en cuanto a la fertilidad del suelo y mejorar así el diseño de planes de fertilización en plantaciones con una superficie relativamente grande. De esta manera, se pueden ajustar planes de fertilización más eficientes a escala de grupos de rodales, como un primer paso hacia la selvicultura de precisión, intensificando y diversificando la gestión en función de las diferencias edáficas. Finalmente, aunque los análisis foliares y de suelos indiquen la existencia de deficiencias nutricionales, la fertilización de las plantaciones no siempre va a producir efectos positivos sobre su crecimiento si no se diseña adecuadamente teniendo en cuenta varios factores que pueden estar influyendo negativamente en dicha respuesta, como la densidad de las plantaciones (sinergias con la programación de los clareos y claras) y la elección de la dosis y del producto a aplicar (habitualmente dosis bajas de N-P-K en lugar de incluir otros nutrientes como Mg, B y Zn o usar otros productos como micorrizas, biofertilizantes etc…). ABSTRACT Teak (Tectona grandis L.f.) has been traditionally considered as a precious wood in SE Asia, where it is indigenous. However, during recent decades the species has reached worldwide relevance in the tropical high quality hardwood sector. Teak has been widely established in Central America, where it has become a key species in the forest sector due to its socioeconomic impact, either because of the big-scale plantations of transnational companies and the abundant small-scale plantations established by many farmers. Despite the relevance of the species, little research has been carried out regarding its soil fertility and nutrition management, a key issue both for sustainability and productivity. The present Thesis performs a literature review to this respect, characterize the soil fertility and the nutrition of teak plantations of Central America and propose several management tools. Soil deficiencies of K and P are usually found in teak plantations in Central America, in addition to occasional acidity problems. These problems are mainly derived of (a) a poor site selection performed during 80s and 90s; and (b) small-scale plantations by farmers in sites which are not adequate for the species. These common soil fertility problems related with P and K soil availability are probably the cause of the relatively low P and K foliar concentration (0,88±0,07% K y 0,16±0,04% P) found in representative teak plantations of the region. Several statistical models are proposed, which allow forest managers to: (a) use them as a reference for foliar analysis interpretation, as they show values considered as representative for teak plantations with an adequate nutritional status in the region; (b) estimate the amount of nutrients accumulated in the aerial biomass of the plantations and, especially, the amount of them which are extracted from the systems as wood is harvested in thinning or final clearcuts. The accumulation of N, P and K result in a key factor for teak management in the region. This turns out to be especially relevant for the P and K because their high output rate by timber extraction and the low soil availability result in an important unbalance which constitutes a risk regarding the sustainability of the system. To this respect, modifying the harvesting time from the usual right now (January-May, business as usual scenario) to September or December (proposed alternatives) can reduce between 24 and 28% the N output associated to timber extraction, 29% the P output and between 14 and 43% the K. Foliar P concentration is a main limiting factor for teak plantations productivity in Central America and a 0.125% critical level is proposed. In addition, the results show a very low tolerance for soil salinity, tendency which was not previously reported. Hence, the probability of teak plantations to have low or very low Site Index is high when Na Saturation is higher than 1.1%. On the other hand, K is confirmed as one of the key nutrients regarding teak nutrition in Central America and a 3.09% provisional critical level is proposed for K Saturation; when values are above this level the probability of having very high Site Index is high. Multivariate statistical analyses have been successfully tested to be used as tools to group forest stands according to their soil fertility similarities. Hence, more efficient fertilization plans can be designed for each group of stands, intensifying and diversifying nutritional management according to soil fertility differences. This methodology, which is considered as a first step towards precision forestry, is regarded as helpful tool to design fertilization plans in big scale plantations. Finally, even though foliar and soil analysis would point out some nutritional deficiencies in a forest stand, the results show how the fertilization is not always going to have a positive effect over forest growth if it is not adequately designed. Some factors have been identified as determinants of tree response to fertilization: density (synergisms between fertilization and thinning scheduling) and the appropriate selection of dosages and product (usually low dosages are applied and N-P-K is preferred instead of applying other nutrients such as Mg, B or Zn or using other alternatives such as mycorrhizas or biofertilizers).