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Published: 4 June 2021
Last updated: 10 March 2023

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1

Pavan, Marcos Antonio. Lições de fertilidade do solo: PH. Londrina, PR: Instituto Agronômico do Paraná, 1997.

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2

Wright, R. J., V. C. Baligar, and R. P. Murrmann, eds. Plant-Soil Interactions at Low pH. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3438-5.

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3

Date, R. A., N. J. Grundon, G. E. Rayment, and M. E. Probert, eds. Plant-Soil Interactions at Low pH: Principles and Management. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-011-0221-6.

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4

Sheppard, M. I. Soil sorption of iodine: Effects of pH and enzymes. Pinawa, Man: Whiteshell Laboratories, 1997.

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5

J, Wright R., Baligar V. C, and Murrmann R. P, eds. Plant-soil interactions at low pH: Proceedings of the Second International Symposium on Plant-Soil Interactions at Low pH, 24-29 June, 1990, Beckley, West Virginia, USA. Dordrecht: Kluwer Academic, 1991.

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6

International Symposium on Plant-Soil Interactions at Low pH (3rd 1993 Brisbane, Qld.). Plant-soil interactions at low pH: Principles and management : proceedings of the Third International Symposium on Plant-Soil Interactions at Low pH, Brisbane, Queensland, Australia, 12-16 September 1993. Dordrecht: Kluwer Academic, 1995.

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7

Karst, Tammy Lynn. Dynamics of soil PH fluctuations in reclaimed land in Coniston, Ontario. Sudbury, Ont: Laurentian University, Department of Biology, 1993.

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8

International Symposium on Plant-Soil Interactions at Low pH (4th 1996 Minas Gerais, Brazil). Plant-soil interactions at low pH: Sustainable agriculture and forestry production : proceedings of the fourth International Symposium on Plant-Soil Interactions at Low pH, Belo Horizonte, Minas Gerais, Brazil, 17-24 March 1996. Campinas: Brazilian Soil Science Society, 1997.

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9

Price, Cynthia B. Transformation of RDX and HMX under controlled Eh/pH conditions. Vicksburg, Miss: U.S. Army Engineer Waterways Experiment Station, 1998.

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10

Gough, L. P. Element concentrations in soils and other surficial materials of Alaska: An account of the concentrations of 43 chemical elements, ash, and pH in soil and other unconsolidated regolith samples. Washington: U.S. G.P.O., 1988.

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11

Gough, L. P. Element concentrations in soils and other surficial materials of Alaska: An account of the concentrations of 43 chemical elements, ash, and pH in soil and other unconsolidated regolith samples. Washington, DC: Dept. of the Interior, 1988.

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12

Dan, Binkley, ed. Acidic deposition and forest soils: Context and case studies of the southeastern U.S. New York: Springer-Verlag, 1989.

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13

Dan, Binkley, ed. Acidic deposition and forest soils: Context and case studies of the southeastern U.S. New York: Springer-Verlag, 1988.

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14

Taggart, Errol L. Particle size distribution, pH and soil moisture content gradients on Inco CD tailings area in Copper Cliff, Ontario. Sudbury, Ont: Laurentian University, Department of Biology, 1996.

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15

Kennedy, Harvey E. Shumard oaks successfully planted on high pH soils. [New Orleans, La.]: U.S. Dept. of Agriculture, Forest Service, Southern Forest Experiment Station, 1986.

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16

Kennedy, Harvey E. Shumard oaks successfully planted on high pH soils. [New Orleans, La.]: U.S. Dept. of Agriculture, Forest Service, Southern Forest Experiment Station, 1985.

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17

Schjørring, Jan K. Planters proton-balance: Indflydelsen af ionoptagelse, kvælstofassimilation og fosformangel på netto-fluxen af protoner mellem rødder og rodmedium, pH i rhizosfæren og udnyttelsen af jord som fosforkilde = Proton balance of plants : influence of ion uptake, nitrogen assimilation, and phosphorus deficiency on the net flux of protons between roots and root medium, rhizosphere pH, and acquisition of phosphorus from soil. København: Afdelingen for planternes ernæring, den Kgl. Veterinær- og landbohøjskole, 1985.

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18

Howat, Darlene. Acceptable salinity, sodicity and pH values for boreal forest reclamation. [Edmonton]: Alberta Environment, Environmental Service, Environmental Sciences Division, 2000.

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19

Tolsted, David N. Liming soils above ph 5.2 does not increase populus growth. [St. Paul, Minn.?]: U.S. Dept. of Agriculture, Forest Service, North Central Forest Experiment Station, 1988.

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20

Tolsted, David N. Liming soils above ph 5.2 does not increase populus growth. [St. Paul, Minn.?]: U.S. Dept. of Agriculture, Forest Service, North Central Forest Experiment Station, 1988.

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21

Tolsted, David N. Liming soils above ph 5.2 does not increase populus growth. [St. Paul, Minn.?]: U.S. Dept. of Agriculture, Forest Service, North Central Forest Experiment Station, 1988.

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22

Tucker, Gary B. pH. IN Williams, R. D.; Schuman, G. E., editors, Reclaiming mine soils and overburden in the western United States--Analytic parameters and procedures. S.l: s.n, 1987.

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23

Baligar, V. C., Robert J. Wright, and R. Paul Murrmann. Plant-Soil Interactions at Low pH. Springer My Copy UK, 1991.

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24

Plant-Soil Interactions at Low pH (Developments in Plant and Soil Sciences). Springer, 2007.

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25

Oshunsanya, Suarau, ed. Soil pH for Nutrient Availability and Crop Performance. IntechOpen, 2019. http://dx.doi.org/10.5772/68057.

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26

Roseberg, Richard J. Chloride fertilizer and soil pH effects on nitrification rate and soil solution constituents. 1985.

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27

Hazelton, Pam, and Brian Murphy. Interpreting Soil Test Results. CSIRO Publishing, 2016. http://dx.doi.org/10.1071/9781486303977.

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Interpreting Soil Test Results is a practical reference enabling soil scientists, environmental scientists, environmental engineers, land holders and others involved in land management to better understand a range of soil test methods and interpret the results of these tests. It also contains a comprehensive description of the soil properties relevant to many environmental and natural land resource issues and investigations. This new edition has an additional chapter on soil organic carbon store estimation and an extension of the chapter on soil contamination. It also includes sampling guidelines for landscape design and a section on trace elements. The book updates and expands sections covering acid sulfate soil, procedures for sampling soils, levels of nutrients present in farm products, soil sodicity, salinity and rainfall erosivity. It includes updated interpretations for phosphorus in soils, soil pH and the cation exchange capacity of soils. Interpreting Soil Test Results is ideal reading for students of soil science and environmental science and environmental engineering; professional soil scientists, environmental scientists, engineers and consultants; and local government agencies and as a reference by solicitors and barristers for land and environment cases.
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28

Date, R. A., N. J. Grundon, and G. E. Rayment. Plant-Soil Interactions at Low pH: Principles and Management. Springer My Copy UK, 1995.

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29

Date, R. A., N. J. Grundon, G. E. Rayment, and M. E. Probert. Plant-Soil Interactions at Low pH : Principles and Management: Proceedings of the Third Intenational Symposium on Plant-Soil Interactions at Low pH, ... Springer, 2013.

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30

Love, Connie Sue. Effect of depth of burial of inoculum and soil pH on cephalosporium stripe of wheat. 1986.

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31

Rayment, George E., and David J. Lyons. Soil Chemical Methods - Australasia. CSIRO Publishing, 2010. http://dx.doi.org/10.1071/9780643101364.

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Soil Chemical Methods – Australasia describes over 200 laboratory and field chemical tests relevant to Australasia and beyond. The information and methodology provided across 20 chapters is comprehensive, systematic, uniquely coded, up-to-date and designed to promote chemical measurement quality. There is guidance on the choice and application of analytical methods from soil sampling through to the reporting of results. In many cases, optional analytical ‘finishes’ are provided, such as flow-injection analysis, electro-chemistry, multiple flame technologies, and alternatives to chemical testing offered by near-range and mid-range infrared diffuse reflectance spectroscopy. The book supersedes and updates the soil chemical testing section of the 1992 Australian Laboratory Handbook of Soil and Water Chemical Methods of Rayment and Higginson, while retaining method codes and other strengths of that Handbook. Chapters cover soil sampling, sample preparation and moisture content; electrical conductivity and redox potential; soil pH; chloride; carbon; nitrogen; phosphorus; sulphur; gypsum; micronutrients; extractable iron, aluminium and silicon; saturation extracts; ion-exchange properties; lime requirements; total miscellaneous elements; miscellaneous extractable elements; alkaline earth carbonates and acid sulfate soils. In addition, there are informative Appendices, including information on the accuracy and precision of selected methods. This book targets practising analysts, laboratory managers, students, academics, researchers, consultants and advisors involved in the analysis, use and management of soils for fertility assessments, land use surveys, environmental studies and for natural resource management.
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32

Baligar, V. C., Robert J. Wright, and R. Paul Murrmann. Plant-Soil Interactions at Low pH: Proceedings of the Second International Symposium on Plant-Soil Interactions at Low pH, 24–29 June 1990, Beckley ... USA. Springer, 2012.

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33

Sugalski, Mark T. Habitat specificity for soil moisture, soil pH, and light intensity by the red-backed salamander, Plethodon cinereus. 1995.

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34

Dept.of Environment. Determination of the PH Value of Sludge, Soil, Mud and Sediment and the Lime Requirement of Soil. 2nd ed. Stationery Office Books, 1992.

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35

Baligar, V. C., Robert J. Wright, and R. Paul Murrmann. Plant-Soil Interactions at Low PH: Proceedings of the Second International Symposium on Plant-Soil Interactions at Low PH, 24-29 June 1990, Beckley West Virginia, USA. Springer, 2012.

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36

Crannell, Wanda K. Soil pH and calcium effects on nodulation of nursery grown red alder. 1993.

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37

Grundon, N. J., M. E. Probert, R. A. Date, and G. E. Rayment. Plant-Soil Interactions at Low PH : Principles and Management: Proceedings of the Third Intenational Symposium on Plant-Soil Interactions at Low PH, Brisbane, Queensland, Australia, 12-16 September 1993. Springer London, Limited, 2012.

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38

Stiles, Carol Maurine. Infection of winter wheat by Cephalosporium gramineum and the effect of soil pH. 1994.

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39

Plant-soil interactions at low pH: Sustainable agriculture and forestry production : Proceedings of the fourth International Symposium on Plant-Soil Interactions ... Minas Gerais, Brazil, 17-24 March 1996. Brazilian Soil Science Society, 1997.

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40

Allen, H. Lee, Philip Schoeneberger, Drew McAvoy, Dan Binkley, and Charles T. Driscoll. Acidic Deposition and Forest Soils: Context and Case Studies of the Southeastern United States. Springer London, Limited, 2012.

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41

Acidic Deposition and Forest Soils: Context and Case Studies of the Southeastern United States. Springer, 2012.

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42

Allen, H. Lee, Philip Schoeneberger, Drew McAvoy, Dan Binkley, and Charles T. Driscoll. Acidic Deposition and Forest Soils: Context and Case Studies of the Southeastern United States (Ecological Studies). Springer, 1989.

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43

Nutrient Solution: Calculation and Formulation of Nutrient Solution in Soil-Less Culture / PH / EC / Hydroponics - Aquaponics - Bioponics - NFT. Independently Published, 2021.

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44

Wilsey, Brian J. Biodiversity of Grasslands. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198744511.003.0002.

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Grasslands can be surprisingly diverse and contain many charismatic flora and fauna. Plant species are often combined into functional groups. Three major conceptual models: competitors-stress tolerants-ruderals (CSR); the leaf traits, plant height, seed mass (LHS); and R*, used to classify grassland species are described by the author. There are three distinct groups of mammalian herbivores based on the ways that herbivores harbor cellulose degrading microbes: hindgut fermentation, foregut fermentation, and foregut fermentation with rumination. Grasslands have a smaller number of bird species than forested systems, and the bird species that are endemic to grasslands tend to be specialized to open habitat (e.g., large flightless birds). Abundant insects can gathered into feeding groups. Single-celled organisms are important in grassland nutrient cycling and as mutualists and pathogens and are extremely abundant in soil. Soil pH is a strong predictor of bacterial diversity (as in plants), with diversity higher in neutral than in acidic soils.
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45

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 phototrophs, but it can have deleterious effects on microbes. In addition to these familiar factors, the small size of microbes sets limits on their physical world. Microbes are said to live in a “low Reynolds number environment”. When the Reynolds number is smaller than about one, viscous forces dominate over inertial forces. For a macroscopic organism like us, moving in a low Reynolds number environment would seem like swimming in molasses. Microbes in both aquatic and terrestrial habitats live in a low Reynolds number world, one of many similarities between the two environments at the microbial scale. Most notably, even soil microbes live in an aqueous world, albeit a thin film of water on soil particles. But the soil environment is much more heterogeneous than water, with profound consequences for biogeochemical processes and interactions among microbes. The chapter ends with a discussion of how the physical-chemical environment of microbes in biofilms is quite different from that of free-living organisms.
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46

Kacorzyk, Piotr. Wartość gospodarcza okrywy roślinnej gleby w aspekcie nawożenia oraz zdolności retencyjnej płytki gleby górskiej. Publishing House of the University of Agriculture in Krakow, 2018. http://dx.doi.org/10.15576/978-83-66602-33-5.

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The aim of the study was to assess the impact of method management of mountain soil on the quantity and quality of waste water, and the amount of mineral nutrients it contains. I have analyzed the water, that was moved through the soil profiles of 0-20 cm and 0-40 cm depth. I have also evaluated the floristic composition, the productivity of grassland and arable land, and the use of fertilizers by vegetation and soil chemical properties. I have found that the type of plant cover of the soil had a significant effect on the amount and chemical composition of water moving through the soil profile. Arable land was characterized by an average of 5 percentage point higher drainage rates compared to meadows. The smallest outflow of water from the soil was found in the first research period (intensive vegetation), and the largest in the third period (non-vegetation). The largest amount of the mineral content carried out annually with a soaking water, was observed on the arable land and was on average more than 2 times larger than on other fertilizers. This evidenced by the greater variation in the composition of floristic vegetation and its productivity. Between 0-20 cm and 0-40 cm of soil profiles, significant differences in the amount of waste water and mineral components were observed. The water drainage coefficient from the shallow profile was on average 9 percentage points higher than from the deeper profile. The amount of the sum of mineral loads, excluding calcium from the shallow soil profile was 94,5% higher than the sum of loads taken from the deeper soil profile. In the unused meadow the improvement of soil chemical properties was observed. There was an increase in pH, and the accumulation of minerals resulted from the positive balance of most of the ingredients.
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47

Bittleston, Leonora S. Commensals of Nepenthes pitchers. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198779841.003.0023.

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Carnivorous Nepenthes pitcher plants contain aquatic ecosystems within each fluid-filled pitcher. Communities of arthropods and microbes colonize pitcher pools, and some organisms are endemic to the pitcher habitat. Flies and mites are the most apparent colonizers, and together with numerous protists, fungi, and bacteria, they form a food web of predators, decomposers, and primary producers. Bacterial diversity and composition are correlated strongly with fluid pH. Closely related organisms co-occur within pitchers, suggesting that competition is not the primary structuring force of pitcher communities. Pitchers are ephemeral habitats when compared with surrounding soil, and the former communities have fewer organisms and are less predictable than the latter. It is still unknown to what extent pitcher plants and their inhabitants influence one another’s fitness.
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48

Rengel, Zdenko. Handbook of Plant Growth pH as the Master Variable (Books in Soils, Plant and the Environment). CRC, 2002.

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49

Fakin, Darinka, Selestina Gorgieva, and Alenka Ojstršek. Ekologija plemenitilnih procesov: Navodila za vaje. University of Maribor Press, 2022. http://dx.doi.org/10.18690/um.fs.7.2022.

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Poseben problem odpadkov v tekstilni industriji predstavljajo odpadne tehnološke vode, predvsem tiste, ki nastajajo pri plemenitenju tekstilij. Te odpadne vode so močno obremenjene, vsebujejo različne kemikalije in tekstilna pomožna sredstva, imajo ekstremne pH-vrednosti in visoke KPK in BPK vrednosti, različne tipe organskih barvil, kar povzroča obarvanost, vsebujejo fosfate, sulfate in ostale soli, tenzide, maščobe in olja ter različne tipe težkih kovin. Tekstilne odpadne vode so zelo heterogene po sestavi, zato je čiščenje takšnih voda kompleksna naloga, za katero ni idealne in v naprej izdelane metode. Glede na proizvodni proces je potrebno izbrati fleksibilno in ekonomsko upravičeno tehnologijo čiščenja. Pri izbiri tehnologije čiščenja odpadnih voda moramo upoštevati njihovo količino in kakovost, ki jo ovrednotimo s specifičnimi in sumarnimi ekološkimi parametri.
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50

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 approaches based on 16S rRNA gene sequencing have revealed that natural microbial communities have a few abundant types and many rare ones. These organisms differ substantially from those that can be grown in the laboratory using cultivation-dependent approaches. The abundant types of microbes found in soils, freshwater lakes, and oceans all differ. Once thought to be confined to extreme habitats, Archaea are now known to occur everywhere, but are particularly abundant in the deep ocean, where they make up as much as 50% of the total microbial abundance. Dispersal of bacteria and other small microbes is thought to be easy, leading to the Bass Becking hypothesis that “everything is everywhere, but the environment selects.” Among several factors known to affect community structure, salinity and temperature are very important, as is pH especially in soils. In addition to bottom-up factors, both top-down factors, grazing and viral lysis, also shape community structure. According to the Kill the Winner hypothesis, viruses select for fast-growing types, allowing slower growing defensive specialists to survive. Cultivation-independent approaches indicate that fungi are more diverse than previously appreciated, but they are less diverse than bacteria, especially in aquatic habitats. The community structure of fungi is affected by many of the same factors shaping bacterial community structure, but the dispersal of fungi is more limited than that of bacteria. The chapter ends with a discussion about the relationship between community structure and biogeochemical processes. The value of community structure information varies with the process and the degree of metabolic redundancy among the community members for the process.
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