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Książki na temat „Ultra high purity oxygen”

Autor: Grafiati

Data publikacji: 27 września 2024

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1

Outlaw, R. A. Permeation of oxygen through high purity, large grain silver. [Washington, D.C.]: National Aeronautics and Space Administration, Scientific and Technical Information Office, 1987.

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2

Waseda, Yoshio, i Minoru Isshiki, red. Purification Process and Characterization of Ultra High Purity Metals. Berlin, Heidelberg: Springer Berlin Heidelberg, 2002. http://dx.doi.org/10.1007/978-3-642-56255-6.

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3

Neuharth, Clark R. Ultra-high-purity silicon for infrared detectors: A materials perspective. Washington, D.C: U.S. Dept. of the Interior, Bureau of Mines, 1989.

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4

Neuharth, Clark R. Ultra-high-purity silicon for infrared detectors: A materials perspective. Washington, DC: Dept. of the Interior, 1989.

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5

Waseda, Yoshio. Purification Process and Characterization of Ultra High Purity Metals: Application of Basic Science to Metallurgical Processing. Berlin, Heidelberg: Springer Berlin Heidelberg, 2002.

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6

Yoshio, Waseda, i Isshiki Minoru 1948-, red. Purification process and characterization of ultra high purity metals: Application of basic science to metallurgical processing. Berlin: Springer-Verlag, 2002.

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7

Ultra high purity fluid: Markets, technologies, players, users. Norwalk, CT: Business Communications Co., 1989.

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8

McWhirter, John R. Use of High-Purity Oxygen in the Activated Sludge. Taylor & Francis Group, 2021.

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9

(Editor), Yoshio Waseda, i Minoru Isshiki (Editor), red. Purification Process and Characterization of Ultra High Purity Metals. Springer, 2001.

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10

Purification Process and Characterization of Ultra High Purity Metals. Island Press, 2001.

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11

Analysis of trace halocarbon contaminants in ultra high purity helium. Moffett Field, Calif: National Aeronautics and Space Administration, Ames Research Center, 1994.

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12

McWhirter, J. R., i Richard Prober, red. The Use of High-purity Oxygen in the Activated Sludge Process. CRC Press, 2019. http://dx.doi.org/10.1201/9780429290718.

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13

McWhirter, J. R. Use of High-Purity Oxygen in the Activated Sludge: Volume 1. Taylor & Francis Group, 2019.

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14

McWhirter, J. R. Use of High-Purity Oxygen in the Activated Sludge: Volume 1. Taylor & Francis Group, 2019.

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15

McWhirter, J. R. Use of High-Purity Oxygen in the Activated Sludge: Volume 1. Taylor & Francis Group, 2019.

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16

McWhirter, J. R. Use of High-Purity Oxygen in the Activated Sludge: Volume 1. Taylor & Francis Group, 2019.

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17

McWhirter, J. R. Use of High-Purity Oxygen in the Activated Sludge: Volume 1. Taylor & Francis Group, 2019.

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18

The Use of high-purity oxygen in the activated sludge process (Water pollution control technology series). CRC Press, 2005.

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19

Isshiki, Minoru, i Yoshio Waseda. Purification Process and Characterization of Ultra High Purity Metals: Application of Basic Science to Metallurgical Processing. Springer Berlin / Heidelberg, 2012.

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20

Lachniet, Matthew S., i Juan Pablo Bernal-Uruchurtu. AD 550–600 Collapse at Teotihuacan. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.003.0006.

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Streszczenie:

We analyze a 2400-year rainfall reconstruction from an ultra-high-resolution absolutely-dated stalagmite (JX-6) from southwestern Mexico (Lachniet et al., 2012). Oxygen isotope variations correlate strongly to rainfall amount in the Mexico City area since 1870 CE, and for the wider southwestern Mexico region since 1948, allowing us to quantitatively reconstruct rainfall variability for the Basin of Mexico and Sierra Madre del Sur for the past 2400 years. Because oxygen isotopes integrate rainfall variations over broad geographic regions, our data suggest substantial variations in Mesoamerican monsoon strength over the past two millennia. As a result of low age uncertainties (≤ 11 yr), our stalagmite paleoclimate reconstruction allows us to place robust ages on past rainfall variations with a resolution an order of magnitude more precise than archeological dates associated with societal change. We relate our new rainfall reconstruction to the sequence of events at Teotihuacan (Millon, 1967; Cowgill, 2015a) and to other pre-Colombian civilizations in Mesoamerica. We observe a centuries long drying trend that culminated in peak drought conditions in ca. 750 CE related to a weakening monsoon, which may have been a stressor on Mesoamerican societies. Teotihuacan is an ideal location to test for links between climate change and society, because it was located in a semi-arid highland valley with limited permanent water sources, which relied upon spring fed irrigation to ensure a reliable maize harvest (Sanders, 1977). The city of Teotihuacan was one of the largest Mesoamerican cities, which apparently reached population sizes of 80,000 to 100,000 inhabitants by AD 300 (Cowgill, 1997; 2015a). Following the “Great Fire”, which dates approximately to AD 550, population decreased to lower levels and many buildings were abandoned (Cowgill, 2015). Because of the apparent reliance on rainwater capture (Linn é, 2003) and spring-fed agriculture in the Teotihuacan valley to ensure food security and drinking water, food production and domestic water supplies should have been sensitive to rainfall variations that recharge the surficial aquifer that sustained spring discharge prior recent groundwater extraction.

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