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1

100 easy-to-grow native plants: For American gardens in temperate zones. Firefly Books, 2009.

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Johnson, Lorraine. 100 easy-to-grow native plants: For American gardens in temperate zones. Firefly Books, 1999.

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Johnson, Lorraine. 100 easy-to-grow native plants: For American gardens in temperate zones. Firefly Books, 2009.

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Johnson, Lorraine. 100 easy-to-grow native plants: For American gardens in temperate zones. Firefly Books, 2009.

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5

Kostiainen, Katri. Wood properties of northern forest trees grown under elevated CO₂, O₃ and temperature. Finnish Society of Forest Science, 2007.

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6

O'Hagan, S. P. Electrical, structural and optical characterisation of gallium arsenide grown by molecular beam epitaxy at low temperature. UMIST, 1995.

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7

Townsend, S. M. The structural electrical and optical characterisation of indium gallium arsenide grown by molecular beam epitaxy atlow temperature. UMIST, 1995.

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8

Lynch, M. A. The structural and electrical characterisation of AlxGax as grown by molecular beam epitaxy at low temperatures. UMIST, 1994.

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9

Clarke, Andrew. Temperature, growth and size. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199551668.003.0013.

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Growth involves two flows of energy. The first is chemical potential energy in the monomers used to construct the proteins, lipids, polysaccharides and nucleic acids forming the new tissue. The second is the metabolic energy (ATP or GTP) used to construct the new tissue; this is the metabolic cost of growth and can be expressed as a dimensionless fraction of the energy retained in the new tissue. Its value is ~0.33. Typical temperature sensitivities for growth in the wild lie in the range Q10 1.5 – 3. Within species there may be evolutionary adjustments to growth rate to offset the effects of
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10

Clarke, Andrew. Global temperature and life. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199551668.003.0014.

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The extreme meteorological surface air temperatures recorded to date are –89.2 oC in Antarctica, and 56.7 oC in Death Valley, California. Ground temperatures can be higher or lower than these air temperatures. The bulk of oceanic water is cold (< 4 oC) and thermally stable. Whilst data on limits to survival attract considerable attention, the thermal limits to completion of the life cycle (which define the limits to life) are much less well known. Currently identified upper thermal limits for growth are 122 oC for archaeans, 100 oC for bacteria and ~60 oC for unicellular eukaryotes. No unic
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11

Sheppard, Charles R. C., Simon K. Davy, Graham M. Pilling, and Nicholas A. J. Graham. Coral reefs. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198787341.003.0001.

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Coral reefs are the ocean’s richest ecosystem in terms of biodiversity and productivity. They are restricted to tropical waters, where conditions of salinity, temperature and sedimentation are suitable. Where they grow, their main benthic organisms deposit substantial limestone skeletons, such that they effectively make their own habitat which sustains their dynamic nature and supports the wide range of species which inhabit them. Reefs grow to the low tide level, thus providing a breakwater, but the richest parts lie 5–20 metres below the surface, an area where light is still sufficient but w
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12

Burt, Stephen, and Tim Burt. Oxford Weather and Climate since 1767. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780198834632.001.0001.

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Oxford Weather and Climate since 1767 provides a detailed description and analysis of the weather records made at the Radcliffe Observatory in Oxford, the longest continuous series of single-site weather records in Britain and one of the longest in the world. The earliest records date from 1767, and daily records are unbroken since November 1813. The records allow the reconstruction of 200-year temperature and rainfall series and places the Oxford records in the context of long-term climate change. In this, the first full publication of the entire dataset, the long Oxford record is both celebr
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13

Loka, Hany. Ultrafast all-optical switching using low-temperature-grown gallium arsenide. 1998.

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14

Zhao, Pin. Characterization and applications of low-temperature-grown MBE gallium arsenides. 1994.

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15

Johnson, Lorraine. 100 Easy-to-Grow Native Plants: For American Gardens in Temperate Zones. Firefly Books, 1999.

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16

Kirchman, David L. Microbial growth, biomass production, and controls. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0008.

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Soon after the discovery that bacteria are abundant in natural environments, the question arose as to whether or not they were active. Although the plate count method suggested that they were dormant if not dead, other methods indicated that a large fraction of bacteria and fungi are active, as discussed in this chapter. It goes on to discuss fundamental equations for exponential growth and logistic growth, and it describes phases of growth in batch cultures, continuous cultures, and chemostats. In contrast with measuring growth in laboratory cultures, it is difficult to measure in natural env
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17

Petherick, Jennifer Sue. Hydrogenated amorphous silicon grown at low temperature using the dc saddle-field deposition system. 2004.

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18

Rez, Peter. The Simple Physics of Energy Use. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198802297.001.0001.

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In industrially developed countries, energy is used primarily for three things—maintaining a comfortable environment in buildings, transporting people and goods and manufacturing products. Each accounts for about one-third of the total primary energy use. Controlling the indoor temperature accounts for most of the energy use in buildings. Therefore, this strongly depends on the local climate. Electricity accounts for a high proportion of the energy transfer in developed countries. The problem is that electricity cannot easily be stored, and that supply therefore has to match demand. This makes
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19

Ellam, Rob. 7. Reconstructing the past and weathering the future. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0007.

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Tiny microfossils called Foraminifera form calcium carbonate shells that record the δ18O composition of the seawater in which they grew. These microfossils are found in sea bed sediment cores, and a lot of information from these oxygen isotope records can be extracted. ‘Reconstructing the past and weathering the future’ looks at the methodology used in palaeoclimate studies and explains gain and phase modelling and Milankovitch orbital cycles. Similar isotope temperature records have been constructed from polar ice cores. Atmospheric CO2 composition can be reconstructed from the amount of CO2
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20

He, Junfeng. Angle-Resolved Photoemission Spectroscopy on High-Temperature Superconductors: Studies of Bi2212 and Single-Layer FeSe Film Grown on SrTiO3 Substrate. Springer, 2016.

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He, Junfeng. Angle-Resolved Photoemission Spectroscopy on High-Temperature Superconductors: Studies of Bi2212 and Single-Layer FeSe Film Grown on SrTiO3 Substrate. Springer, 2018.

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22

Beerling, David. The Emerald Planet. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780192806024.001.0001.

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Global warming is contentious and difficult to measure, even among the majority of scientists who agree that it is taking place. Will temperatures rise by 2ºC or 8ºC over the next hundred years? Will sea levels rise by 2 or 30 feet? The only way that we can accurately answer questions like these is by looking into the distant past, for a comparison with the world long before the rise of mankind. We may currently believe that atmospheric shifts, like global warming, result from our impact on the planet, but the earth's atmosphere has been dramatically shifting since its creation. This book reve
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23

Centre, Bhabha Atomic Research, ed. Study of hydride blisters grown on Zr-2.5Nb pressure tube spool piece under simulated condition of in-reactor pressure and temperature. Bhabha Atomic Research Centre, 2005.

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24

Schuerger, Andrew Conrad. Effects of temperature and hydrogen ion concentration on disease caused by Fusarium solani f. sp. phaseoli in Vigna radiata grown in hydroponic nutrient solution. 1991.

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25

Lindenmayer, David, Damian Michael, Mason Crane, et al. Wildlife Conservation in Farm Landscapes. CSIRO Publishing, 2016. http://dx.doi.org/10.1071/9781486303113.

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An increasing number of Australians want to be assured that the food and fibre being produced on this continent have been grown and harvested in an ecologically sustainable way. Ecologically sustainable farming conserves the array of species that are integral to key ecological processes such as pollination, seed dispersal, natural pest control and the decomposition of waste. 
 Wildlife Conservation in Farm Landscapes communicates new scientific information about best practice ways to integrate conservation and agriculture in the temperate eucalypt woodland belt of eastern Australia. It is
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26

Kirchman, David L. Community structure of microbes in natural environments. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0004.

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Community structure refers to the taxonomic types of microbes and their relative abundance in an environment. This chapter focuses on bacteria with a few words about fungi; protists and viruses are discussed in Chapters 9 and 10. Traditional methods for identifying microbes rely on biochemical testing of phenotype observable in the laboratory. Even for cultivated microbes and larger organisms, the traditional, phenotype approach has been replaced by comparing sequences of specific genes, those for 16S rRNA (archaea and bacteria) or 18S rRNA (microbial eukaryotes). Cultivation-independent appro
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