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Статті в журналах з теми "Environment and Earth Sciences"
Sousa, C. "Inquiry learning for gender equity using History of Science in Life and Earth Sciences’ learning environments." Multidisciplinary Journal for Education, Social and Technological Sciences 3, no. 1 (March 22, 2016): 84. http://dx.doi.org/10.4995/muse.2016.3762.
Повний текст джерелаNaeher, Sebastian, Xingqian Cui, and Roger E. Summons. "Biomarkers: Molecular Tools to Study Life, Environment, and Climate." Elements 18, no. 2 (April 1, 2022): 79–85. http://dx.doi.org/10.2138/gselements.18.2.79.
Повний текст джерелаWenceslau, Eliza C., and Joseli M. Piranha. "Earth system sciences and permaculture: contributions to environmental." Terrae Didatica 14, no. 4 (October 30, 2018): 363–68. http://dx.doi.org/10.20396/td.v14i4.8653827.
Повний текст джерелаViktor, Iakovlev, and Galianov Aleksei. "Mining sciences in the branch of Earth sciences." Izvestiya vysshikh uchebnykh zavedenii. Gornyi zhurnal, no. 1 (February 17, 2021): 9–14. http://dx.doi.org/10.21440/0536-1028-2021-1-9-14.
Повний текст джерелаIakovlev, Viktor. "Mining sciences in the branch of Earth sciences." Izvestiya vysshikh uchebnykh zavedenii. Gornyi zhurnal, no. 1 (February 17, 2021): 5–14. http://dx.doi.org/10.21440/0536-1028-2021-1-5-14.
Повний текст джерелаAllègre, Claude, and Vincent Courtillot. "Revolutions in the earth sciences." Philosophical Transactions of the Royal Society of London. Series B: Biological Sciences 354, no. 1392 (December 29, 1999): 1915–19. http://dx.doi.org/10.1098/rstb.1999.0531.
Повний текст джерелаOmar Riyad Al-Qaqah and Hussein Abdellateef Ba'arah. "The Degree to Which Earth and Environmental Science Teachers Practice Twenty-First-Century Skills in Jordan." Britain International of Humanities and Social Sciences (BIoHS) Journal 4, no. 3 (November 2, 2022): 531–42. http://dx.doi.org/10.33258/biohs.v4i3.785.
Повний текст джерелаSharma, Rekha. "VEDIC SCIENCE AND ENVIRONMENT." International Journal of Research -GRANTHAALAYAH 3, no. 9SE (September 30, 2015): 1–4. http://dx.doi.org/10.29121/granthaalayah.v3.i9se.2015.3165.
Повний текст джерелаKevles, Daniel J. "The contested Earth: science, equity & the environment." Daedalus 137, no. 2 (April 2008): 80–95. http://dx.doi.org/10.1162/daed.2008.137.2.80.
Повний текст джерелаWang, Ning, Robert J. Stern, Mary L. Urquhart, and Katherine M. Seals. "Google Earth Geoscience Video Library (GEGVL): Organizing Geoscience Videos in a Google Earth Environment to Support Fieldwork Teaching Methodology in Earth Science." Geosciences 12, no. 6 (June 15, 2022): 250. http://dx.doi.org/10.3390/geosciences12060250.
Повний текст джерелаДисертації з теми "Environment and Earth Sciences"
Black, Benjamin A. (Benjamin Alexander). "Volatiles as a link between planetary interiors and the environment." Thesis, Massachusetts Institute of Technology, 2013. http://hdl.handle.net/1721.1/84920.
Повний текст джерелаCataloged from PDF version of thesis.
Includes bibliographical references (pages 163-179).
Volatiles derived from planetary interiors influence magma evolution and environmental processes. Over appropriate timescales, Earth's mantle, crust, ocean, and atmosphere constitute coupled systems. The apparently synchronous Siberian Traps eruption and end-Permian mass extinction offer an ideal test case to study the interactions between magmatism and climate. In this thesis, I use experimental petrology, numerical modeling, geochemical measurements, and field observations to investigate the petrologic sources, eruptive transfer, and climatic effects of volatiles released during emplacement of the Siberian large igneous province. In an extreme variation on terrestrial volatile cycling, I also explore the erosional history of Titan as recorded in valley networks carved by rivers of liquid hydrocarbons.
by Benjamin A. Black.
Ph.D.
Johnson, Sarah Stewart. "Mars in the late Noachian : evolution of a habitable surface environment." Thesis, Massachusetts Institute of Technology, 2008. http://hdl.handle.net/1721.1/45605.
Повний текст джерелаThis electronic version was submitted by the student author. The certified thesis is available in the Institute Archives and Special Collections.
Includes bibliographical references.
This dissertation addresses whether simple life forms might have existed on Mars during the late Noachian epoch, and whether those life forms, or their traces, can be detected today. It begins by analyzing the ancient Martian climate in light of new evidence that sulfur chemistry played a prominent role in the planet's early evolution. It finds that sulfur-induced greenhouse warming could have periodically heated the planet enough to support liquid water, thereby creating warm, wet, clement conditions. Moreover, it finds that those warming pulses, while short-lived over geologic time, may have persisted for hundreds of years. If sulfur helped create environmental conditions capable of hosting life, however, it also created conditions that were adverse to sustaining it. In particular, dissipation of sulfur volatiles cooled the climate, and sulfur rainout contributed to the acidity of Martian surface waters. The dissertation therefore proceeds to analyze the potential for persistence and detection of life in terrestrial environments with Mars-like characteristics. It first investigates the potential for detecting ancient life by searching for lipid biomarkers in sulfur-rich acid salt lakes, concluding that a variety of biomarkers may be more resistant to decay than previously believed. It then analyzes soil samples from permafrost, discovering the oldest independently authenticated viable organisms ever found, and positing low-level metabolic activity and DNA repair as a survival mechanism in ancient cells. Finally, the dissertation uses deep sequencing to examine prokaryotic diversity in a terrestrial Mars-like river characterized by low pH and high concentrations of iron and sulfur, with results considered in light of the implications for life detection approaches incorporating new, in situ "PCR in a chip" technology. The dissertation concludes by proposing future work, including the ultimate goal of developing a life detection instrument for Mars.
by Sarah Stewart Johnson.
Ph.D.
Mloszewski, Aleksandra. "Environmental and microstructural controls of short-term shell degradation in temperate, macrotidal environments." Thesis, McGill University, 2009. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=40807.
Повний текст джерелаL’état de préservation des coquilles d’organismes marins dépend directement des conditions environnementales dans lesquelles elles se dégradent. Cette étude a pour but de déterminer les conditions de dégradation progressive de coquillages (Mytilus edulis) et de cristaux abiotiques d’aragonite déployés à l’interface eau-sédiment ainsi qu’enfouis (à 10-20 cm) durant treize mois, dans les zones haute et moyenne d’un marais salant, une plage et une crique de la Baie de Fundy (NB, Canada). Les changements macroscopiques, microscopiques et de masse sont discutés relativement aux conditions environnementales. Nos résultats montrent que: 1) la dégradation et les processus agissent très tôt après la déposition, et produisent des changement d’état significatifs en deçà de 13 mois post-mortem. 2) Dans les environments ci-dessus, la mue des tablettes de nacre de la surface de la coquille est le processus le plus efficace, suivi par la bioérosion, et la macération. 3) La dissolution joue un rôle secondaire durant la dégradation précoce des coquillages.
Dunn-Sigouin, Etienne. "Evaluation of northern hemisphere blocking climatology in the global environment multiscale (GEM) model and in the present and future climate as simulated by the CMIP5 models." Thesis, McGill University, 2012. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=110589.
Повний текст джерелаLes performances du modele Global Environment Multiscale (GEM), qui est le modele numerique operationel Canadien, a reproduire les variabilites atmospheriques de basse frequence sont evaluees en premier lieu dans le contexte de la climatologie de bloquage atmospherique dans l'hemisphere Nord. Afin de valider le modele, un algorithme de detection de bloquage qui est a la fois comprehensif et relativement simple est applique aux donnees atmospheriques. Les resultats montrent que la frequence maximum de bloquage au dessus de l'Atlantique Nord et l'Europe de l'Ouest est generalement sous-estimee et il y un delai dans la saison d'amplitude maximale puisqu'elle se produit au printemps au lieu de tard en hiver. De plus, la frequence de bloquage est generalement sur-estimee au dessus du Pacifique Nord. Il a ete trouve que les erreurs dans la frequence de bloquage sont grandement associees aux erreurs dans la circulation climatologique de l'atmosphere. En fait, les ondes stationnaires modelisees montrent un delai saisonnier dans le nombre d'onde zonal 1 et un deplacement vers l'Est des composantes du nombre d'onde zonal 2. Ayant confiance en la capacite de notre index pour identifier des bloquages atmospheriques, nous appliquons notre methodologie sur des analyses preliminaires de bloquage climatologique dans l'hemisphere Nord a partir d'un sous-ensemble de modeles climatologiques faisant partie du Coupled Model Inter-Comparison Project Phase 5 (CMIP5). Les integrations historiques revelent que la frequence maximale de bloquage sur l'Euro-Atlantique est generalement sous-estimee durant la saison froide et que la sur-estimation de la frequence maximale de bloguage sur le Pacifique se produit tout au long de l'annee dans certains modeles. En comparaison, les integrations de type RCP8.5 montrent un leger indice d'une reduction de la frequence de bloquage sur le Pacifique meme si aucune tendance significative en terme de duree de bloquage n'a ete trouvee.
Meredith, Laura Kelsey 1982. "Field measurement of the fate of atmospheric H₂ in a forest environment : from canopy to soil." Thesis, Massachusetts Institute of Technology, 2013. http://hdl.handle.net/1721.1/79283.
Повний текст джерелаCataloged from PDF version of thesis.
Includes bibliographical references (p. 245-254).
Atmospheric hydrogen (H₂ ), an indirect greenhouse gas, plays a notable role in the chemistry of the atmosphere and ozone layer. Current anthropogenic emissions of H₂ are substantial and may increase with its widespread use as a fuel. The H₂ budget is dominated by the microbe-mediated soil sink, and although its significance has long been recognized, our understanding is limited by the low temporal and spatial resolution of traditional field measurements. This thesis was designed to improve the process-based understanding of the H₂ soil sink with targeted field and lab measurements. In the field, ecosystem-scale flux measurements of atmospheric H₂ were made both above and below the forest canopy for over a year using a custom, automated instrument at the Harvard Forest. H₂ fluxes were derived using a flux-gradient technique from the H₂ concentration gradient and the turbulent eddy coefficient. A ten-fold improvement in precision was attained over traditional systems, which was critical for quantifying the whole ecosystem flux from small H2 concentration gradients above the turbulent forest canopy. Soil uptake of atmospheric H₂ was the dominant process in this forest ecosystem. Rates peaked in the summer and persisted at reduced levels in the winter season, even across a 70 cm snowpack. We present correlations of the H₂ flux with environmental variables (e.g., soil temperature and moisture). This work is the most comprehensive attempt to elucidate the processes controlling biosphere-atmosphere exchange of H₂ . Our results will help reduce uncertainty in the present-day H₂ budget and improve projections of the response of the H₂ soil sink to global change. In the lab, we isolated microbial strains of the genus Streptomyces from Harvard Forest and found that the genetic potential for atmospheric H₂ uptake predicted H₂ consumption activity. Furthermore, two soil Actinobacteria were found to utilize H₂ only during specific lifecycle stages. The lifecycle of soil microorganisms can be quite complex as an adaptation to variable environmental conditions. Our results indicate that H₂ may be an important energetic supplement to soil microorganisms under stress. These results add to the understanding of the connections between the environment, organismal life cycle, and soil H₂ uptake.
by Laura Kelsey Meredith.
Ph.D.
Chan, Gabriel Angelo Sherak. "Trade and the environment : the political economy of CO₂ emission leakage with analysis of the steel and oil sands industries." Thesis, Massachusetts Institute of Technology, 2009. http://hdl.handle.net/1721.1/115466.
Повний текст джерелаThesis: S.B., Massachusetts Institute of Technology, Department of Political Science, 2009.
Cataloged from PDF version of thesis.
Includes bibliographical references (pages 113-116).
Introduction: In 2007, scientists and governmental officials from around the world contributed to the United Nations-authorized Intergovernmental Panel on Climate Change's (IPCC) Fourth Assessment Report. Through peer-reviewed scientific research and governmental review, the IPCC came to the conclusion that "warming of the climate system is unequivocal," and that "most of the observed increase in global average temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations." The IPCC Fourth Assessment states that humans have "more likely than not" contributed to the phenomena of more frequent "warm spells/heat waves," larger "area[s] affected by droughts," more "intense tropical cyclones.. .and heavy precipitation events," and "extreme high sea level[s]." Citing "high agreement" and "much evidence," the IPCC states that "with current climate change mitigation policies and related sustainable development practices, global GHG [greenhouse gas] emissions will continue to grow over the next few decades." (Intergovernmental Panel on Climate Change, 2007)
by Gabriel A. Chan.
S.B.
Rapopo, Mafusi. "Petrogenesis of the syntectonic Matok Pluton in the Limpopo Belt (South Africa) and its implications of the geodynamic environment." Thesis, Stellenbosch : Stellenbosch University, 2011. http://hdl.handle.net/10019.1/17993.
Повний текст джерелаENGLISH ABSTRACT: The ~2.67 Ga Matok pluton comprises calc‐alkaline pyroxene (px)‐bearing and px‐free granitoids. The pluton was constructed by means of two episodes of intrusion each of which had co‐magmatic px‐bearing and px‐free granitoid groups. All the granitoid groups (px‐bearing and px‐free) are characterised by non‐porphyritic and porphyritic varieties. The phenocrysts in both episodes of intrusion are plagioclase ± alkali feldspar and are aligned parallel to the trend of the Limpopo Belt, attesting to a syntectonic emplacement. The time gap between the first and second intrusion is insignificant and magma was most likely stored in the chamber after the first intrusion. Petrography and geochemical signature of both px‐bearing and px‐free granitoid samples have been studied and a petrogenetic model which accounts for the coeval px‐bearing and px‐free granitoids is proposed. The relevance of the syntectonic emplacement of the Matok pluton ie n the Limpopo Belt is also addrssed. Px‐bearing granitoids always have clinopyroxene but orthopyroxene is not always present. Magnetite and ilmenite are present in both px‐bearing and px‐free granitoids but are more abundant in the px‐bearing granitoids and subordinate in the px‐free granitoids. Plagioclase in both px‐bearing and px‐free granitoids is of oligoclase (An12‐30) composition but is relatively more calcic and increases in modal abundance in the px‐bearing granitoids. Alkali feldspar is more dominant in the px‐free granitoids. Hornblende is present in all the px‐bearing granitoids and the px‐free granitoids with ≤71 wt.% SiO2 but is absent in the px‐free granites with >71 wt.% SiO2. Both magmatic epidote and titanite occur exclusively in the px‐free granitoids with ≤71 wt.% SiO2 and are absent in all the px‐bearing granitoids as well as the px‐free gra nites with >71 wt.% SiO2. Px‐bearing granitoids are mainly of dioritic and granodioritic and have subordinate granitic composition while px‐free granitoids are mainly of granitic and granodioritic and have subordinate dioritic composition. All the rocks define well correlated variation of SiO2 with the rest of the major elements. However, there is always a hiatus between the granites with >71 wt.% SiO2 and all other rocks. Px‐bearing and px‐free granitoids at the same SiO2 concentrations tend to have approximately equal concentrations of MgO, CaO and TiO2, whereas K2O concentration is distinctively higher for the px‐free granitoids. The distribution of the high field strength elements (HFSE; Nb, Ta, Zr and Hf) and rare earth elements (REE) is similar in both px‐bearing and px‐free granitoids. On contrary, Th, U, Cs and Rb are characteristically higher in the px‐free granitoids. All granitoids are characterised by negative anomalies of the HFSE (Nb, Ta and Ti) and the LILE (Th, U and Sr) on primitive mantle normalised diagrams. On the one hand, concentrations of compatible elements (Cr, Ni and Mg) in the Matok pluton granitoids are rather low for a mantle source. On the other hand, all the granitoids have superchondtritic Nb/Ta ratios that overlap with those of the Ventersdorp continental flood basalts which extruded in the Kaapvaal Craton at ~2.7 Ga. The continental crust typically has subchondritic Nb/Ta ratio, and superchondtritic Nb/Ta ratios are widely accepted to resemble a mantle source. The implication is that the Matok pluton granitoids had inherited the superchondtritic Nb/Ta ratio from their source; juvenile underplated mafic magmas that had ponded owing to the impact of the Ventersdorp mantle plume. The large volumes of ponded magma s probably induced the high grade metamorphism in the Limpopo Belt. All the granitoids of the Matok pluton are probably products of one partial melting event. One possible way to account for the co‐existence of px‐bearing and px‐free granitoids in the Matok pluton is by means of, at least, two magma chambers; one which was filled with anhydrous magma and the other which was filled with hydrous magma. An alternative model would be that in which there was only one chamber. In the one chamber scenario, the magma was hydrodynamically sorted into zones that differed mostly in fH2O and concentrations of highly fluid‐mobile elements but conserved the uniformity in fluid immobile elements. Regardless of the number of chambers, magma batches intruded in the form of feeder dikes which minimally interacted, thus avoiding the hydration of pyroxene in the px‐bearing granitoids.
SELELEKELA: Plutone ya Matok e fumanehang profinsing ya Limpopo sebakeng seo ho digeologist se tsebahalang ka hore ke Lebanta la Limpopo e ile ya aheya dilemong tse 2.67 biliyone tse fetileng. Plutone ena eile ya aheya ka mekgahlelo e mmeli, mme mokgahlelo ka mong o ne o bopilwe ka majwe a nang le pyroxene le a senang yona. Majwe kaofela ke a mofuta wa calc‐alkaline. Phapang e kgolo dipakeng tsa mefuta ena e mmedi ya majwe ke boteng ba pyroxene le boteng ba epidote le titanite majweng a nang le pyroxene le a senang pyroxene ka ho latellana. Ha e le diminerale tse ding kaofela tsona ha likgethe mofuta wa lejwe; liteng mefuteng ya majwe ka bobedi. Kgonahalo ya hore plutone ya Matok e ahwe ka mefuta ena e mmedi (px‐bearing and px‐free) e tlile ka mekgoa e mmedi kapa o mong wa mekgwa ena yo ka bobedi e ka etsahalang. (1)Tlaase semelong sa lesheleshele moralla (magma) hone ho ena le didiba tse pedi, seseng se tshetse lesheleshele le chesang haholo ebile le le metsi a fokolang (anhydrous magma) ha se seng se ne se tshetse lesheleshele le metsi a mangata (hydrous magma). Ho tloheng moo didibeng tse pedi ho tla moo plutone ea Matok eleng teng kajeno masheleshele ana a ne a tla ka mokgwa wa di‐dike tseo kaofela phello ya tsona e neng e le sebakeng se le seng‐plutone ya Matok. (2) Mokgwa wa bobedi ke haeba ho ne ho ena le sediba se le seng sa lesheleshele moralla, mme ka sedibeng ka moo ho ne ho ena le maqulwana (zones) a neng a fapane ka bongata ba metsi. Ho tloha sedibeng moo masheleshele ana a ne a tloha ka bona boqulwana boo entse ele ka mokhwa wa di‐dike, mme kaofela phello ya di‐dike ene ele plutone ya Matok. Kaofela majwe a plutone ya Matok a na le feldspar eo boholo ba nako e patlameng ho ya nqa bophirimela‐bochabela (W‐E), e leng nqa eo Lebanta la Limpopo le phatlaletseng ka teng. Hona ho tiisa hore plutone ya Matok e aheile nakong yo Lebanta la Limpopo le neng le ntse le aheya le lona. Ke dilemong tse kabang 2.7 biliyone tse fetileng ha dikarolong tse ding tsa Cratone ya Kaapvaal ho ne ho aheya majwe a moralla a Ventersdorp. Majwe ana ke a hlahang tlaase botebong ba lefatshe (mantle), mme a susumeditswe ke plumo. Karolo boholo ya lesheleshele moralla hae ya ka ya nyoloha ho fihla hodimo lefatsheng. Empa mofuthu o mongata ho nyoloha leshelesheleng moo ke ona oileng wa 'pheha' majwe ho phatlalla le Lebanta la Limpopo. Ho nyoloha hona ha plumo ho etsahetse ka nako e lengwe le ho tsukutleha ho hoholo ho potapota le Cratone ya Kalahari, mme bobedi diketsahalo tsena diile tsa tswala Lebanta la Limpopo. Hobane plutone ya Matok e aheile hanghang ka mora hore lesheleshele la moralla le dule tlaase ho lekgapetla la lefatshe (crust), dielemente tse ratang haholo diminerale tsa ditemperetjha tse hodimo diile tsa feela jwalo di nkile lefa hotswa lesheleshele moralleng la Ventersdorp.
Wilkinson, John L. "Occurrence, bioaccumulation, fate and transport of pharmaceuticals, plasticisers, illicit drugs and perfluorinated compounds in the aquatic environment." Thesis, Kingston University, 2017. http://eprints.kingston.ac.uk/39283/.
Повний текст джерелаAdelman, Jessica. "Mineral interactions in a gold mining environment: change in oxidation rate of stibnite as affected by the addition of varying amounts of pyrite in an oxygenated flow through system." Thesis, McGill University, 2010. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=92390.
Повний текст джерелаOn croit qu'un des mécanismes importants de dissolution de la stibnite (Sb₂S₃) dans les résidus miniers est par contact avec un minéral ayant un plus fort potentiel électrique, tel que la pyrite (FeS₂). L'objectif de la recherche était de déterminer l'impact du ratio stibnite vs. pyrite et l'effet du pH sur le taux de dissolution de la stibnite. Quatre essais de lessivage en colonnes ont été réalisés. Les deux premiers essais de lessivage avec de l'eau déionisée ont montré que le traitement contenant la plus forte proportion de pyrite (95% pyrite) a résulté en la plus grand quantité cumulative de Sb dissous (Exp #2-16730 mg Sb/kg stibnite). L'analyse spectroscopique par absorption des rayons-X (XANES) de la phase solide a révélé que la proportion de Sb total sous forme Sb(V)-O était plus importante dans le traitement 95% pyrite comparé à tous les autres traitements mixtes et au traitement contrôle de 100% stibnite. Ces observations indiquent que des interactions galvaniques ont eu lieu entre la stibnite et la pyrite. En utilisant une solution tamponnée à pH 7.5, il fut possible de déterminer l'effet d'un pH légèrement alcalin sur ces interactions entre la stibnite et la pyrite. Dans ces conditions, la quantité maximale de Sb dissous a été atteinte dans le traitement 95% pyrite (Exp #3-18090 mg Sb/kg stibnite), ce qui est comparable au traitement 95% pyrite dans l'expérience #2 de lessivage à l'eau. Cependant, l'analyse XANES a révélé une proportion moindre du Sb total sous forme d'oxide dans l'essai de lessivage à pH 7.5, possiblement en raison de la formation d'un complexe soluble entre Sb et HCO₃-. L'expérience #4 a testé l'impact de l'arsenopyrite sur la dissolution de la stibnite lors d'un lessivage à l'eau. Dans ce cas, le traitement 95% arsenopyrite (Exp #4-10311 mg Sb/kg stibnite) a libéré moins de Sb en solution comparé au traitement 95% pyrite de l'expérience #2, et ce résultat s'explique par la plus p
Williams, Jeni Kimberly. "Inquiry learning in the earth science classroom." CSUSB ScholarWorks, 2004. https://scholarworks.lib.csusb.edu/etd-project/2641.
Повний текст джерелаКниги з теми "Environment and Earth Sciences"
Jonathan, Turk, ed. Earth science and the environment. 4th ed. Belmont, CA: Thomson Brooks/Cole, 2007.
Знайти повний текст джерелаJonathan, Turk, ed. Earth science and the environment. 2nd ed. Fort Worth: Saunders College Pub., 1999.
Знайти повний текст джерелаThompson, Graham R. Earth science and the environment. Fort Worth: Saunders College Pub., 1995.
Знайти повний текст джерелаJonathan, Turk, ed. Earth science and the environment. Fort Worth, TX: Saunders College Pub., Harcourt Brace Jovanovich College Publishers, 1993.
Знайти повний текст джерелаJonathan, Turk, ed. Earth science and the environment. 3rd ed. Belmont, CA: Thomson Brooks/Cole, 2005.
Знайти повний текст джерелаNational Geographic Society (U.S.) and Glencoe/McGraw-Hill, eds. Earth science: Geology, the environment, and the universe. New York, N.Y: Glencoe/McGraw-Hill, 2005.
Знайти повний текст джерелаJohnson, Matthew S. (Matthew Stanley), 1966-, ed. Chemistry and the environment. New York: Cambridge University Press, 2012.
Знайти повний текст джерелаGroundwater in the environment: An introduction. Malden, MA: Blackwell Pub., 2007.
Знайти повний текст джерелаSarre, Philip. One world for one earth: Saving the environment. Sterling, VA: Earthscan, 2009.
Знайти повний текст джерелаPaul, Smith, and Morris Eleanor, eds. One world for one earth: Saving the environment. London: Earthscan Publications in association with the Open University, 1991.
Знайти повний текст джерелаЧастини книг з теми "Environment and Earth Sciences"
Kumar Maity, Swapan, and Ramkrishna Maiti. "Environment of Sediment Deposition." In SpringerBriefs in Earth Sciences, 39–55. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-71315-1_3.
Повний текст джерелаHamacher, H., B. Fitton, and J. Kingdon. "The Environment of Earth-Orbiting Systems." In Fluid Sciences and Materials Science in Space, 1–50. Berlin, Heidelberg: Springer Berlin Heidelberg, 1987. http://dx.doi.org/10.1007/978-3-642-46613-7_1.
Повний текст джерелаTrauth, Martin H., and Elisabeth Sillmann. "Scientific Information in Earth Sciences." In Springer Textbooks in Earth Sciences, Geography and Environment, 1–14. Berlin, Heidelberg: Springer Berlin Heidelberg, 2018. http://dx.doi.org/10.1007/978-3-662-56203-1_1.
Повний текст джерелаTrauth, Martin H. "Data Acquisition in Earth Sciences." In Springer Textbooks in Earth Sciences, Geography and Environment, 1–14. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-74913-2_1.
Повний текст джерелаTrauth, Martin H., and Elisabeth Sillmann. "Visualizing 2D Data in Earth Sciences." In Springer Textbooks in Earth Sciences, Geography and Environment, 99–118. Berlin, Heidelberg: Springer Berlin Heidelberg, 2018. http://dx.doi.org/10.1007/978-3-662-56203-1_5.
Повний текст джерелаTrauth, Martin H., and Elisabeth Sillmann. "Visualizing 3D Data in Earth Sciences." In Springer Textbooks in Earth Sciences, Geography and Environment, 119–42. Berlin, Heidelberg: Springer Berlin Heidelberg, 2018. http://dx.doi.org/10.1007/978-3-662-56203-1_6.
Повний текст джерелаTrauth, Martin H. "Data Analysis in the Earth Sciences." In Springer Textbooks in Earth Sciences, Geography and Environment, 1–8. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07719-7_1.
Повний текст джерелаBakke, Jostein, and Øyvind Paasche. "Sediment Core and Glacial Environment Reconstruction." In Encyclopedia of Earth Sciences Series, 979–84. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2642-2_471.
Повний текст джерелаZou, Hao, Shou-Ting Zhang, Min Li, and Zhan-Zhang Xu. "Petrological Characteristics and Sedimentary Environment." In Modern Approaches in Solid Earth Sciences, 65–76. Singapore: Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-7562-1_3.
Повний текст джерелаLemoalle, Jacques. "Lake Chad: A Changing Environment." In NATO Science Series: IV: Earth and Environmental Sciences, 321–39. Dordrecht: Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-94-007-0967-6_13.
Повний текст джерелаТези доповідей конференцій з теми "Environment and Earth Sciences"
Maldonado, Carlos A., and Andrew D. Ketsdever. "Drag Measurements in a Simulated Low-Earth Orbit Environment." In 53rd AIAA Aerospace Sciences Meeting. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2015. http://dx.doi.org/10.2514/6.2015-1392.
Повний текст джерела"Flood Vulnerability Classification of Lafia Township, Nasarawa State, Nigeria." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214016.
Повний текст джерела"Dynamic of Reproductive Qualities of Japanese Quails." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214033.
Повний текст джерела"Regulation of Second Messenger Signaling in Hypoxic Neonatal Rats: Effect of Glucose, Oxygen and Epinephrine Resuscitation." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214035.
Повний текст джерела"Microblological Quality Assessment of Meat Samples Sold In Kaura Namoda." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214058.
Повний текст джерела"Linkage Model between Sustainable Consumption and Household Waste Management System." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214068.
Повний текст джерела"Locating Suitable Sites for Construction of Underground Dams through Analytic Hierarchy Process." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214072.
Повний текст джерела"Green Buildings." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214074.
Повний текст джерела"A Future Prospect for Domestic Waste Management in Qatar." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214080.
Повний текст джерела"A comparison of vegetation composition within and surrounding gravel borrow pit sites around Gaborone, Botswana." In International Conference on Earth, Environment and Life sciences. International Institute of Chemical, Biological & Environmental Engineering, 2014. http://dx.doi.org/10.15242/iicbe.c1214088.
Повний текст джерелаЗвіти організацій з теми "Environment and Earth Sciences"
Davis, J. C., L. Younker, I. Proctor, B. Bannevik, D. Layton, K. Jackson, and J. Hannon. Protecting environment, national security, and health, earth and environment sciences 1996 annual report. Office of Scientific and Technical Information (OSTI), January 1996. http://dx.doi.org/10.2172/643281.
Повний текст джерелаDavis, J. Protecting environment, national security, and health earth and environmental sciences 1997 annual report. Office of Scientific and Technical Information (OSTI), April 1998. http://dx.doi.org/10.2172/2643.
Повний текст джерелаCoblentz, David. Earth and Environmental Sciences (EES) Division Solid Earth Programs. Office of Scientific and Technical Information (OSTI), June 2013. http://dx.doi.org/10.2172/1083092.
Повний текст джерелаYounker, L. Earth and environmental sciences annual report 1998. Office of Scientific and Technical Information (OSTI), May 1999. http://dx.doi.org/10.2172/15173.
Повний текст джерелаAuthor, Not Given. Earth and Environmental Sciences Area Strategic Vision 2025. Office of Scientific and Technical Information (OSTI), March 2017. http://dx.doi.org/10.2172/1344535.
Повний текст джерелаYonker, L., and B. Dannevik. Earth and Environmental Sciences 1999 Annual Report Meeting National Needs. Office of Scientific and Technical Information (OSTI), July 2000. http://dx.doi.org/10.2172/791660.
Повний текст джерелаGeernaert, Gary, Shaima Nasiri, Jeff Stehr, Ashley Williamson, Sally McFarlane, Rick Petty, Xujing Davis, et al. Biological and Environmental Research, Earth and Environmental Systems Sciences Division (formerly Climate and Environmental Sciences Division) Strategic Plan: 2018–2023. Office of Scientific and Technical Information (OSTI), May 2018. http://dx.doi.org/10.2172/1616535.
Повний текст джерелаIatsyshyn, Andrii, Anna Iatsyshyn, Valeriia Kovach, Iryna Zinovieva, Volodymyr Artemchuk, Oleksandr Popov, Olha Cholyshkina, Oleksandr Radchenko, Oksana Radchenko, and Anastasiia Turevych. Application of Open and Specialized Geoinformation Systems for Computer Modelling Studying by Students and PhD Students. [б. в.], November 2020. http://dx.doi.org/10.31812/123456789/4460.
Повний текст джерелаVoisin, Nathalie, Andrew Bennett, Yilin Fang, Grey Nearing, Bart Nijssen, and Yuhan Rao. A science paradigm shift is needed for Earth and Environmental Systems Sciences (EESS) to integrate Knowledge-Guided Artificial Intelligence (KGAI) and lead new EESS-KGAI theories. Office of Scientific and Technical Information (OSTI), April 2021. http://dx.doi.org/10.2172/1769651.
Повний текст джерелаYounker, L. W., and S. J. Peterson. Earth Sciences report, 1989--1990. Edited by M. E. Price. Office of Scientific and Technical Information (OSTI), March 1991. http://dx.doi.org/10.2172/5455473.
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