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Books on the topic 'Physical-chemical attributes of the soil'

Author: Grafiati

Published: 4 June 2021

Last updated: 18 February 2022

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1

Kinetics of soil chemical processes. Academic Press, 1989.

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2

Remediation of petroleum contaminated soils: Biological, physical, and chemical processes. Lewis Publishers, 1998.

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3

Andrén, Olof. Spatial variation of soil physical and chemical properties in an arable field with high clay content. Sveriges lantbruksuniversitet, Institutionen för ekologi och miljövård, 1990.

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4

Rourke, R. V. Chemical and physical properties of the Mapleton, Monson, Saddleback, and Sisk soil map units. Department of applied Ecology and Environmental Sciences, University of Maine, 1998.

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5

Rourke, R. V. Chemical and physical properties of the Mapleton, Monson, Saddleback, and Sisk soil map units. Dept. of Applied Ecology and Environmental Sciences, University of Maine, 1998.

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6

Rourke, R. V. Chemical and physical properties of the Danforth, Elliottsville, Peacham and Penquis soil map units. Department of applied Ecology and Environmental Sciences, University of Maine, 1997.

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7

Rourke, R. V. Chemical and physical properties of the Aurelie, Burnham, Easton, Lille, Linneus, Monadnock, Nicholville, and Tunbridge soil map units. Dept. of Plant and Soil Sciences, University of Maine, 1990.

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8

Lieberman, Davine M. Pre- and post-operational effects of a temperature control device on physical, chemical, and biological attributes of Shasta Lake, California: Phase 1, spring 1995 through fall 1997. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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9

Marron, D. C. Field and laboratory data describing physical and chemical characteristics of metal-contaminated flood-plain deposits downstream from lead, west-central South Dakota. Dept. of the Interior, U.S. Geological Survey, 1988.

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10

Marron, D. C. Field and laboratory data describing physical and chemical characteristics of metal-contaminated flood-plain deposits downstream from lead, west-central South Dakota. Dept. of the Interior, U.S. Geological Survey, 1988.

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11

Nazarov, Vyacheslav, Roman Sandu, and Dmitriy Makarenkov. Technique and technology of combined processing of solid waste. INFRA-M Academic Publishing LLC., 2020. http://dx.doi.org/10.12737/996365.

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The educational manual provides information about industrial and domestic waste. The properties of the lithosphere and the soil components. The estimation of soil pollution by industrial and household waste. The peculiarities of classification of wastes and provides criteria for determining risk. Describe the General pattern of the combined methods of processing that use mechanical, physical, thermal and biothermal recycling processes. In detail the construction described granulating equipment, methods of intensification of processes, process flow sheets and engineering calculation methods. Sp

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12

1933-, Sumner M. E., and Stewart B. A. 1932-, eds. Soil crusting: Chemical and physical processes. Lewis Publishers, 1992.

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13

Sparks, Donald L., Ph. D., Suarez Donald L, and Soil Science Society of America. Division S-1., eds. Rates of soil chemical processes. Soil Science Society of America, 1991.

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14

Sumner, Malcolm E. Soil Crusting: Chemical and Physical Processes (Advances in Soil Science). Lewis Publishers, 1992.

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15

Wright, C. Harold. A Handbook of Soil Analysis ; Physical and Chemical Methods. Logos Press, 1994.

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16

H, Loeppert Richard, Schwab A. Paul, Goldberg Sabine, and Soil Science Society of America. Division S-1., eds. Chemical equilibrium and reaction models. Soil Science Society of America, 1995.

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17

(Editor), Donald L. Sparks, Soil Science Society of America (Corporate Author), and American Society of Agronomy (Corporate Author), eds. Methods of Soil Analysis. Part 3. Chemical Methods (Soil Science Society of America Book Series, No. 5). American Society of Agronomy-Soil Science Society of America, 1996.

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18

Sparks, Donald L. Rates of Soil Chemical Processes: Proceedings of a Symposium Sponsored by Divisions S-1, S-2, S-3, and S-9 of the Soil Science Society of America in (S S S a Special Publication). Soil Science Society of Amer, 1991.

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19

L, Brusseau Mark, ed. Innovative subsurface remediation: Field testing of physical, chemical, and characterization technologies. American Chemical Society, 1999.

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20

Kirchman, David L. The physical-chemical environment of microbes. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198789406.003.0003.

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Many physical-chemical properties affecting microbes are familiar to ecologists examining large organisms in our visible world. This chapter starts by reviewing the basics of these properties, such as the importance of water for microbes in soils and temperature in all environments. Another important property, pH, has direct effects on organisms and indirect effects via how hydrogen ions determine the chemical form of key molecules and compounds in nature. Oxygen content is also critical, as it is essential to the survival of all but a few eukaryotes. Light is used as an energy source by photo

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21

Veblen, Thomas, Kenneth Young, and Antony Orme. The Physical Geography of South America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195313413.001.0001.

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The Physical Geography of South America, the eighth volume in the Oxford Regional Environments series, presents an enduring statement on the physical and biogeographic conditions of this remarkable continent and their relationships to human activity. It fills a void in recent environmental literature by assembling a team of specialists from within and beyond South America in order to provide an integrated, cross-disciplinary body of knowledge about this mostly tropical continent, together with its high mountains and temperate southern cone. The authors systematically cover the main components

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22

(Editor), Mark L. Brusseau, David A. Sabatini (Editor), John S. Gierke (Editor), and Michael D. Annable (Editor), eds. Innovative Subsurface Remediation: Field Testing of Physical, Chemical, and Characterization Technologies (Acs Symposium Series). An American Chemical Society Publication, 1999.

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23

A, Shmalzer Paul, and John F. Kennedy Space Center., eds. Soil, groundwater, surface water, and sediments of Kennedy Space Center, Florida: Background chemical and physical characteristics. National Aeronautics and Space Administration, John F. Kennedy Space Center, 2000.

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24

1951-, Wilson S. A., and Geological Survey (U.S.), eds. The physical preparation and chemical analysis of NIST SRMs 2786 and 2787, lead paint in soil. U.S. Dept. of the Interior, U.S. Geological Survey, 1995.

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25

Soil, groundwater, surface water, and sediments of Kennedy Space Center, Florida: Background chemical and physical characteristics. National Aeronautics and Space Administration, John F. Kennedy Space Center, 2000.

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26

A, Poesen J. W., Nearing M. A, and International Society of Soil Science., eds. Soil surface sealing and crusting: Selected papers of the International Symposium on Soil Crusting: Chemical and Physical Processes, May 30-June 1, 1991, Athens, Georgia, USA. Catena Verlag, 1993.

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27

Roitberg, Bernard D. Chemical communication. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198797500.003.0010.

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Communication takes place when two or more individuals interact via signal release and reception. This chapter focuses on chemical communication among arthropods, first, discussing the physical attributes of chemical communication and following up with examples that demonstrate the importance of chemical communication as a mediator of behavioral, ecological and evolutionary processes. In doing so, both the functional (i.e. why) and causal (i.e. how) aspects of chemical communication are considered. The examples are drawn from a broad range of topics, including mating conflict (and resolution),

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28

Wessel, W. W. Metal Nutrient Dynamics in the Organic Surface Layer of an Acidifying Forest Soil "Modeling the Interaction of Physical, Chemical and Biological Processes". Academisch Proefeschrift, 1997.

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29

J, Horn Michael, United States. Bureau of Reclamation, and Geological Survey (U.S.), eds. Pre- and post-operational effects of a temperature control device on physical, chemical, and biological attributes of Shasta Lake, California: Phase 1, spring 1995 through fall 1997. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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30

Pre- and post-operational effects of a temperature control device on physical, chemical, and biological attributes of Shasta Lake, California: Phase 1, spring 1995 through fall 1997. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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31

J, Horn Michael, United States. Bureau of Reclamation., and Geological Survey (U.S.), eds. Pre- and post-operational effects of a temperature control device on physical, chemical, and biological attributes of Shasta Lake, California: Phase 1, spring 1995 through fall 1997. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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32

J, Horn Michael, United States. Bureau of Reclamation, and Geological Survey (U.S.), eds. Pre- and post-operational effects of a temperature control device on physical, chemical, and biological attributes of Shasta Lake, California: Phase 1, spring 1995 through fall 1997. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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33

J, Horn Michael, United States. Bureau of Reclamation, and Geological Survey (U.S.), eds. Pre- and post-operational effects of a temperature control device on physical, chemical, and biological attributes of Shasta Lake, California: Phase 1, spring 1995 through fall 1997. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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34

J, Horn Michael, United States. Bureau of Reclamation, and Geological Survey (U.S.), eds. Pre- and post-operational effects of a temperature control device on physical, chemical, and biological attributes of Shasta Lake, California: Phase 1, spring 1995 through fall 1997. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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35

J, Horn Michael, United States. Bureau of Reclamation., and Geological Survey (U.S.), eds. Pre- and post-operational effects of a temperature control device on physical, chemical, and biological attributes of Shasta Lake, California: Phase 1, spring 1995 through fall 1997. U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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36

Geological Survey (U.S.), ed. Field and laboratory data describing physical and chemical characteristics of metal-contaminated flood-plain deposits downstream from lead, west-central South Dakota. Dept. of the Interior, U.S. Geological Survey, 1988.

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37

Stirling, Graham, Helen Hayden, Tony Pattison, and Marcelle Stirling. Soil Health, Soil Biology, Soilborne Diseases and Sustainable Agriculture. CSIRO Publishing, 2016. http://dx.doi.org/10.1071/9781486303052.

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Our capacity to maintain world food production depends heavily on the thin layer of soil covering the Earth's surface. The health of this soil determines whether crops can grow successfully, whether a farm business is profitable and whether an enterprise is sustainable in the long term. Farmers are generally aware of the physical and chemical factors that limit the productivity of their soils but often do not recognise that soil microbes and the soil fauna play a major role in achieving healthy soils and healthy crops. Soil Health, Soil Biology, Soilborne Diseases and Sustainable Agricul

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38

Selim, Hussein Magd Eldin, 1944- and Sparks, Donald L., Ph. D., eds. Physical and chemical processes of water and solute transport/retention in soils: Proceedings of a symposium sponsored by Divisions S-1 and S-2 of the Soil Science Society of America in Baltimore, MD, 18 to 22 October 1998. Soil Science Society of America, 2001.

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39

Australian Soil Fertility Manual. CSIRO Publishing, 2006. http://dx.doi.org/10.1071/9780643100725.

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The Australian Soil Fertility Manual is a trusted guide to the safe use and handling of fertilizers. It describes the types of agricultural soils, how they are classified and the interaction of soil, water and nutrients. It also provides an insight into how plants utilise nutrients and the role that individual nutrients play in the process of plant growth. This edition has been revised to reflect an increased emphasis on the environmental fate of nutrients and appropriate management strategies. It also has additional information on soil physical, chemical, and biological properties and d

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40

Pereira, Paulo, Jorge Mataix-Solera, Xavier Úbeda, Guillermo Rein, and Artemi Cerdà, eds. Fire Effects on Soil Properties. CSIRO Publishing, 2019. http://dx.doi.org/10.1071/9781486308149.

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Wildland fires are occurring more frequently and affecting more of Earth's surface than ever before. These fires affect the properties of soils and the processes by which they form, but the nature of these impacts has not been well understood. Given that healthy soil is necessary to sustain biodiversity, ecosystems and agriculture, the impact of fire on soil is a vital field of research. Fire Effects on Soil Properties brings together current research on the effects of fire on the physical, biological and chemical properties of soil. Written by over 60 international experts in the field,

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41

Martin, Colin. Wreck-Site Formation Processes. Edited by Ben Ford, Donny L. Hamilton, and Alexis Catsambis. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780199336005.013.0002.

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The environmental settings within which shipwrecks occur are matters of chance rather than of choice. It is primarily the wreck and not its physical context that is of consequence to nautical archaeologists. No two wreck-site formations are the same, since the complex and interacting variables that constitute the environmental setting, the nature of the ship, and the circumstances of its loss combine to create a set of attributes unique to each site. The dynamic phase, which begins with the event of shipwreck, is characterized by the wreck's status as an environmental anomaly. It is unstable,

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42

White, Robert E. Understanding Vineyard Soils. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780199342068.001.0001.

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The first edition of Understanding Vineyard Soils has been praised for its comprehensive coverage of soil topics relevant to viticulture. However, the industry is dynamic--new developments are occurring, especially with respect to measuring soil variability, managing soil water, possible effects of climate change, rootstock breeding and selection, monitoring sustainability, and improving grape quality and the "typicity" of wines. All this is embodied in an increased focus on the terroir or "sense of place" of vineyard sites, with greater emphasis being placed on wine quality relative to quanti

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43

Parlange, Marc B., and Jan W. Hopmans. Vadose Zone Hydrology. Oxford University Press, 1999. http://dx.doi.org/10.1093/oso/9780195109900.001.0001.

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The vadose zone is the region between ground level and the upper limits of soil fully saturated with water. Hydrology in the zone is complex: nonlinear physical, chemical, and biological interactions all affect the transfer of heat, mass, and momentum between the atmosphere and the water table. This book takes an interdisciplinary approach to vadose zone hydrology, bringing together insights from soil science, hydrology, biology, chemistry, physics, and instrumentation design. The chapters present state-of-the-art research, focusing on new frontiers in theory, experiment, and management of soi

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44

McKenzie, Neil, David Jacquier, Ray Isbell, and Katharine Brown. Australian Soils and Landscapes. CSIRO Publishing, 2004. http://dx.doi.org/10.1071/9780643100732.

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This essential reference provides an introduction to the remarkable soils and landscapes of Australia. It reveals their great diversity and explains why an understanding of soil properties and landscape processes should guide our use of the land. Using striking photographs of characteristic landscapes, it begins by describing the basic properties of soils and how Australia's distinctive soils and landscapes have co-evolved. We gain a greater understanding of why particular soils occur at certain locations and how soil variation can influence landscape processes, agricultural productivity

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45

Hazelton, Pam, and Brian Murphy. Understanding Soils in Urban Environments. CSIRO Publishing, 2011. http://dx.doi.org/10.1071/9780643101432.

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Soil properties such as water retention, salinity and acidity are not just issues for agriculture and forestry. They are equally as significant in creating environmental and structural problems for buildings and other engineering works. As an increasing proportion of the world's population is living in cities, and building and related infrastructure development continues, these problems assume ever-greater importance. In addition, existing works contribute to urban soil erosion and pollution as well as increased levels of urban runoff. Understanding Soils in Urban Environments explains h

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46

Scott, Keith, and Colin Pain, eds. Regolith Science. CSIRO Publishing, 2009. http://dx.doi.org/10.1071/9780643098268.

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This comprehensive reference on the fundamentals of regolith geoscience describes how regolith is developed from parental rocks and emphasises the importance of chemical, physical, water and biological processes in regolith formation. It provides details for mapping regolith landforms, as well as objective information on applications in mineral exploration and natural resource management. Regolith Science also provides a concise history of weathering through time in Australia. It includes previously unpublished information on elemental abundances in regolith materials along with detailed infor

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47

Jacobsen, Dean, and Olivier Dangles. High altitude waters in the face of climate change. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0008.

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Chapter 8 focuses on the effects of warming and changes in precipitation patterns on aquatic life at high altitude. Located near the edge of their climatic limits, in regions where the rate of warming is generally amplified compared with lowlands, high altitude aquatic systems present a high sensitivity to climate change. Changes in mountain climate create a number of indirect effects on aquatic life through the control of hydrological systems and processes, particularly those associated with the cryosphere (e.g. permafrost and ice melting) and the soil–vegetation interface (e.g. treeline expa

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48

Mazzolai, Barbara. Growth and tropism. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780199674923.003.0009.

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Plants or plant parts, such as roots or leaves, have the capacity of moving by growing in response to external stimuli with high plasticity and morphological adaptation to the environment. This chapter analyses some plant features and how they have been translated in artificial devices and control. A new generation of ICT hardware and software technologies inspired from plants is described, which includes an artificial root-like prototype that moves in soil imitating the sloughing mechanism of cells at the root apex level; as well as innovative osmotic-based actuators that generate movement im

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49

Singh, Balwant, Marta Camps-Arbestain, and Johannes Lehmann, eds. Biochar. CSIRO Publishing, 2017. http://dx.doi.org/10.1071/9781486305100.

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Interest in biochar among soil and environment researchers has increased dramatically over the past decade. Biochar initially attracted attention for its potential to improve soil fertility and to uncouple the carbon cycle, by storing carbon from the atmosphere in a form that can remain stable for hundreds to thousands of years. Later it was found that biochar had applications in environmental and water science, mining, microbial ecology and other fields. Beneficial effects of biochar and its environmental applications cannot be fully realised unless the chemical, physical, structural an

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50

Romanowski, Nick. Wetland Weeds. CSIRO Publishing, 2011. http://dx.doi.org/10.1071/9780643103962.

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This comprehensive guide to wetland weeds covers both native and introduced species, ranging from minor or localised environmental problems to those that should not be tolerated in any situation. The author takes a pragmatic approach to weed control, recognising that some weeds may not be possible to eradicate, and emphasising the need to assess the extent and future potential of any infestation before taking action. Weed control should be planned in the context of the overall management goals for any type of wetland, the types of habitat weeds provide or overrun, and whether they can be

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