Academic literature on the topic 'Soils Soils Soil microbiology'

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Journal articles on the topic "Soils Soils Soil microbiology"

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McDaniel, Marshall D., Marcela Hernández, Marc G. Dumont, Lachlan J. Ingram, and Mark A. Adams. "Disproportionate CH4 Sink Strength from an Endemic, Sub-Alpine Australian Soil Microbial Community." Microorganisms 9, no. 3 (March 15, 2021): 606. http://dx.doi.org/10.3390/microorganisms9030606.

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Soil-to-atmosphere methane (CH4) fluxes are dependent on opposing microbial processes of production and consumption. Here we use a soil–vegetation gradient in an Australian sub-alpine ecosystem to examine links between composition of soil microbial communities, and the fluxes of greenhouse gases they regulate. For each soil/vegetation type (forest, grassland, and bog), we measured carbon dioxide (CO2) and CH4 fluxes and their production/consumption at 5 cm intervals to a depth of 30 cm. All soils were sources of CO2, ranging from 49 to 93 mg CO2 m−2 h−1. Forest soils were strong net sinks for CH4, at rates of up to −413 µg CH4 m−2 h−1. Grassland soils varied, with some soils acting as sources and some as sinks, but overall averaged −97 µg CH4 m−2 h−1. Bog soils were net sources of CH4 (+340 µg CH4 m−2 h−1). Methanotrophs were dominated by USCα in forest and grassland soils, and Candidatus Methylomirabilis in the bog soils. Methylocystis were also detected at relatively low abundance in all soils. Our study suggests that there is a disproportionately large contribution of these ecosystems to the global soil CH4 sink, which highlights our dependence on soil ecosystem services in remote locations driven by unique populations of soil microbes. It is paramount to explore and understand these remote, hard-to-reach ecosystems to better understand biogeochemical cycles that underpin global sustainability.
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Eskov, Alen K., Alexei O. Zverev, and Evgeny V. Abakumov. "Microbiomes in Suspended Soils of Vascular Epiphytes Differ from Terrestrial Soil Microbiomes and from Each Other." Microorganisms 9, no. 5 (May 11, 2021): 1033. http://dx.doi.org/10.3390/microorganisms9051033.

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Microbial biodiversity parameters for tropical rainforests remain poorly understood. Whilst the soil microbiome accounts up to 95% of the total diversity of microorganisms in terrestrial ecosystems, the microbiome of suspended soils formed by vascular epiphytes remains completely unexplored. Samples of ground and suspended soils were collected in Cat Tien National Park, southern Vietnam. DNA extraction and sequencing were performed, and libraries of 16s rDNA gene sequences were analyzed. Alpha diversity indices of the microorganisms were the highest in the forest ground soil. In general, the microbiological diversity of all the soil types was found to be similar at the phylum level. Taxonomic composition of the bacterial communities in the suspended soils of plants from the same species are not closer than the taxonomic compositions of the communities in the suspended soils of different plant species. However, the beta diversity analysis revealed significant differences in the movement of mineral elements in terrestrial versus suspended soils. Our data showed that the suspended soils associated with vascular epiphytes were a depository of unique microbiological biodiversity. A contributing factor was the presence of large amounts of organic matter in the suspended soils—deposits collected by the epiphytes—which would have been degraded by termites if it had reached the ground. Further, the nutrient content of the suspended soils was prime for soil respiration activity and taxonomic microbial community biodiversity.
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Czarny, Jakub, Justyna Staninska-Pięta, Jolanta Powierska-Czarny, Jacek Nowak, Łukasz Wolko, and Agnieszka Piotrowska-Cyplik. "Metagenomic Analysis of Soil Bacterial Community and Level of Genes Responsible for Biodegradation of Aromatic Hydrocarbons." Polish Journal of Microbiology 66, no. 3 (September 27, 2017): 345–52. http://dx.doi.org/10.5604/01.3001.0010.4865.

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The aim of the studies was to compare the composition of soil bacterial metabiomes originating from urbanized areas and areas con¬taminated with hydrocarbons with those from agricultural soil and forest soil obtained from a protected wild-life park area. It should be noted that hydrocarbons are everywhere therefore bacteria capable of their utilization are present in every soil type. In the hydrocarbon-contaminated soil and in the soil of anthropogenic origin, the bacteria belonging to Gammaproteobacteria were dominant (28.4–36.6%), whereas in the case of agricultural soil and protected wild-life park soil their ratios decreased (22.8–23.0%) and were similar to that of Alphaproteobacteria. No statistically significant changes were observed in terms of the Operational Taxonomic Unit identified in the studies soils, however, based on the determined alpha-diversity it can be established that contaminated soils were characterized by lower biodiversity indices compared to agricultural and forest soils. Furthermore, the dioxygenase level was also evaluated in the studied soils, which are genes encoding crucial enzymes for the decomposition of mono- and polycyclic aromatic hydrocarbons during the biodegradation of diesel oil (PAHRHDαGN, PAHRHDαGP, xylE, Cat 2,3, ndoB). It was concluded that both the population structure of the soil metabiome and the number of genes crucial for biodegradation processes differed significantly between the soils. The level of analysed genes showed a similar trend, as their highest number in relations to genes encoding 16S RNA was determined in urban and hydrocarbon-contaminated soil.
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Lee, Jung Yeop, and Byung Kook Hwang. "Diversity of antifungal actinomycetes in various vegetative soils of Korea." Canadian Journal of Microbiology 48, no. 5 (May 1, 2002): 407–17. http://dx.doi.org/10.1139/w02-025.

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Diversity of actinomycetes and their antifungal activities against some plant pathogenic fungi were examined in various vegetative soils from 14 different sites in the western part of Korea. Actinomycete counts ranged from 1.17 × 106to 4.20 × 106cfu·g-1dried soil. A total of 1510 actinomycetes were isolated from the soil samples. Streptomyces was predominant in soils with a pH range of 5.1-6.5, 9.1-13.0% moisture, and 9.1-11.0% organic matter. Most Micromonospora, Dactylosporangium, and Streptosporangium were distributed in soils with pH 4.0-5.0, 2.0-9.0% moisture, and 4.0-7.0% organic matter. Actinomadura and nocardioform actinomycetes were abundant in soils with pH 4.0-5.0 and 13.1-20.0% moisture and with 9.1-11.0 and 4.0-7.0% organic matter, respectively. Populations of Streptomyces were predominant in all the soils, but were highest in grassland and lowest in mountain-forest soils. Micromonospora was most abundant in pepper-field soil and nocardioform actinomycetes were highest in rice paddy field soil. Dactylosporangium was predominant in lake-mud sediments and pepper-field soil, Streptosporangium in lake-mud sediments, and Actinomadura in mountain-forest soil. Antifungal actinomycetes were abundant in orchard soil and lake mud. More than 50% of antifungal isolates from most soils were classified as genus Streptomyces. Actinomycete isolates that showed strong antifungal activity against Alternaria mali, Colletotrichum gloeosporioides, Fusarium oxysporum f.sp. cucumerinum, and Rhizoctonia solani were predominant in pepper-field soils, whereas those against Magnaporthe grisea and Phytophthora capsici were abundant in radish-field soils.Key words: actinomycetes, antifungal activity, plant pathogenic fungi, vegetative soils.
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Cullings, Ken, and Shilpa Makhija. "Ectomycorrhizal Fungal Associates of Pinus contorta in Soils Associated with a Hot Spring in Norris Geyser Basin, Yellowstone National Park, Wyoming." Applied and Environmental Microbiology 67, no. 12 (December 1, 2001): 5538–43. http://dx.doi.org/10.1128/aem.67.12.5538-5543.2001.

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ABSTRACT Molecular methods and comparisons of fruiting patterns (i.e., presence or absence of fungal fruiting bodies in different soil types) were used to determine ectomycorrhizal (EM) associates of Pinus contorta in soils associated with a thermal soil classified as ultra-acidic to extremely acidic (pH 2 to 4). EM were sampled by obtaining 36 soil cores from six paired plots (three cores each) of both thermal soils and forest soils directly adjacent to the thermal area. Fruiting bodies (mushrooms) were collected for molecular identification and to compare fruiting body (above-ground) diversity to below-ground diversity. Our results indicate (i) that there were significant decreases in both the level of EM infection (130 ± 22 EM root tips/core in forest soil; 68 ± 22 EM root tips/core in thermal soil) and EM fungal species richness (4.0 ± 0.5 species/core in forest soil; 1.2 ± 0.2 species/core in thermal soil) in soils associated with the thermal feature; (ii) that the EM mycota of thermal soils was comprised of a small set of dominant species and included very few rare species, while the EM mycota of forest soils contained a few dominant species and several rare EM fungal species; (iii) that Dermocybe phoenecius and a species of Inocybe, which was rare in forest soils, were the dominant EM fungal species in thermal soils; (iv) that other than the single Inocybe species, there was no overlap in the EM fungal communities of the forest and thermal soils; and (v) that the fungal species forming the majority of the above-ground fruiting structures in thermal soils (Pisolithus tinctorius, which is commonly used in remediation of acid soils) was not detected on a single EM root tip in either type of soil. Thus, P. tinctorius may have a different role in these thermal soils. Our results suggest that this species may not perform well in remediation of all acid soils and that factors such as pH, soil temperature, and soil chemistry may interact to influence EM fungal community structure. In addition, we identified at least one new species with potential for use in remediation of hot acidic soil.
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Ibekwe, A. Mark, Sharon K. Papiernik, Catherine M. Grieve, and Ching-Hong Yang. "Quantification of Persistence ofEscherichia coliO157:H7 in Contrasting Soils." International Journal of Microbiology 2011 (2011): 1–11. http://dx.doi.org/10.1155/2011/421379.

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Persistence ofEscherichia coli (E. coli)O157:H7 in the environment is a major concern to vegetable and fruit growers where farms and livestock production are in close proximity. The objectives were to determine the effects of preplant fumigation treatment on the survival ofE. coliO157:H7 in two soils and the effects of indigenous bacterial populations on the survival of this pathogen. Real-time PCR and plate counts were used to quantify the survival ofE. coliO157:H7 in two contrasting soils after fumigation with methyl bromide (MeBr) and methyl iodide (MeI). Ten days after fumigation,E. coliO157:H7 counts were significantly lower () in fumigated soils than in the non-fumigated. Direct comparison between MeBr and MeI within each soil indicated that these two fumigants showed similar impacts onE. coliO157:H7 survival. Microbial species diversity as determined by DGGE was significantly higher in clay soil than sandy soil and this resulted in higher initial decline in population in clay soil than in sandy soil. This study shows that if soil is contaminated withE. coliO157:H7, fumigation alone may not eliminate the pathogen, but may cause decrease in microbial diversity which may enhance the survival of the pathogen.
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Mahaney, William C., Jessica Zippin, Michael W. Milner, Kandiah Sanmugadas, R. G. V. Hancock, Susan Aufreiter, Sean Campbell, et al. "Chemistry, mineralogy and microbiology of termite mound soil eaten by the chimpanzees of the Mahale Mountains, Western Tanzania." Journal of Tropical Ecology 15, no. 5 (September 1999): 565–88. http://dx.doi.org/10.1017/s0266467499001029.

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Subsamples of termite mound soil used by chimpanzees for geophagy, and topsoil never ingested by them, from the forest floor in the Mahale Mountains National Park, Tanzania, were analysed to determine the possible stimulus or stimuli for geophagy. The ingested samples have a dominant clay texture equivalent to a claystone, whereas the control samples are predominantly sandy clay loam or sandy loam, which indicates that particle size plays a significant role in soil selection for this behaviour. One potential function of the clays is to bind and adsorb toxins. Although both termite mound and control samples have similar alkaloid-binding capacities, they are in every case very high, with the majority of the samples being above 80%. The clay size material (<2 μm) contains metahalloysite and halloysite, the latter a hydrated aluminosilicate (Al2Si2O4·nH2O), present in the majority of both the termite mound soil and control soil samples.Metahalloysite, one of the principal ingredients found in the pharmaceutical Kaopectate™, is used to treat minor gastric ailments in humans. The soils commonly ingested could also function as antacids, as over half had pH values between 7.2 and 8.6. The mean concentrations of the majority of elements measured were greater in the termite mound soils than in the control soils. The termite mound soils had more filamentous bacteria, whereas the control soils contained greater numbers of unicellular bacteria and fungi.
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Chen, Danmei, Yuqi Duan, Yan Jin, Yuhong Yang, and Ling Yuan. "Soil quality and microbiology in response to fertilizations in a paddy-upland rotation with multiple crops and frequent tillage." Experimental Agriculture 56, no. 2 (October 14, 2019): 227–38. http://dx.doi.org/10.1017/s0014479719000322.

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AbstractBoth short- and long-term effects of fertilizers on crops and soils are often studied only in arid or paddy soils, whereas less is known about the long-term effects in paddy-upland rotations, particularly with multiple crops and frequent tillage in subtropical areas. Therefore, an 18-year field experiment was initialized to assess the effects of different types of fertilization (no fertilizer; chemical fertilizer (CF); and manure in combination with CF (MCF)) on yield and soil chemical and microbial properties in a crop rotation involving rice (Oryza sativa L., summer), rapeseed (Brassica campestris L., winter), tobacco (Nicotiana tabacum L., the following summer), and hairy vetch (Vicia villosa Roth, the following winter). MCF caused higher yields of rapeseed grains and tobacco leaves than CF after 3 or 4 years of implementing the experiment, while rice yields varied little between MCF and CF, with one exception in 2011. Compared with the initial soil properties, providing soil with MCF increased organic matter (OM), while the opposite trend was found with CF. Higher microbial biomasses, enzyme activities, bacterial operational taxonomic units, and richness and diversity indexes of bacterial communities were found in soils receiving MCF, implying the improvement of soil microbial properties in the paddy-upland rotation system with multiple crops and frequent tillage. The experimental soils under varying fertilization were dominated by four bacterial phyla (Proteobacteria, Acidobacteria, Actinobacteria, and unclassified groups), which accounted for approximately 70% of the 16S rDNA sequences. Among the top 20 predominant bacteria, 14 were commonly found in all soil samples irrespective of which fertilizer treatment was implemented. Thus, the presence of those bacteria was stable in the soil and to some extent was influenced by fertilization. Most of them were facultative anaerobic bacteria, which can adapt to both anaerobic paddy soil and aerobic drylands. The dominant bacteria at various taxonomic levels found in soils might reflect multiple soil processes such as OM turnover, nutrient cycling, physical structure formation, and xenobiotic detoxification.
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Martin, S. Bruce, G. S. Abawi, and H. C. Hoch. "The relation of population densities of the antagonist, Laetisaria arvalis, to seedling diseases of table beet incited by Pythium ultimum." Canadian Journal of Microbiology 32, no. 2 (February 1, 1986): 156–59. http://dx.doi.org/10.1139/m86-031.

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Sclerotia of Laetisaria arvalis were added to raw or steamed table beet field soils infested with Pythium ultimum and other low-temperature Pythium spp. to determine the relationship between soil population densities of the antagonist to disease incidence. Decrease in disease incidence of table beet seedlings and final Pythium spp. inoculum densities were linearly related to increasing population density of the antagonist in raw field soils. In P. ultimum infested steamed soils, decreasing disease incidence was also related to increasing population densities of L. arvalis, but the relationship was curvilinear and was described by a quadratic model. The latter models also described the decrease in P. ultimum inoculum densities with increasing levels of the antagonist. Percentages of healthy plants (those surviving the pre- and post-emergence damping-off disease phases) were increased approximately 20% in raw soils containing 100 sclerotia of L. arvalis per gram soil in comparison with those of unamended soils. However, in Pythium infested steamed soils, percentages of healthy plants in soil amended with 100 sclerotia of L. arvalis per gram soil were increased by 40–60%.
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de Freitas, J. R., J. J. Schoenau, S. M. Boyetchko, and S. A. Cyrenne. "Soil microbial populations, community composition, and activity as affected by repeated applications of hog and cattle manure in eastern Saskatchewan." Canadian Journal of Microbiology 49, no. 9 (September 1, 2003): 538–48. http://dx.doi.org/10.1139/w03-069.

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A field site near Humboldt, Saskatchewan, was annually treated with hog or cattle manure and cropped to canola, spring wheat, barley, and canola from 1997 to 2000. During each growing season, soil was analyzed for microbial populations in terms of activity and community structure, and crops were assessed for root rot and foliar diseases. Microbial activity in soils treated with cattle manure was higher than in soils treated with hog manure or urea. Similarly, nitrous oxide emissions from soil increased with increasing rates of hog and cattle manure. Potential human pathogens, including Rahnella, Serratia, Proteus, Leclercia, and Salmonella species, were identified in soils that received cattle manure, whereas pseudomonads were the dominant species in the hog-manure-treated soil. Fecal coliforms were confirmed in soils that received hog or cattle manure. However, Enterobacteriaceae populations were 10-fold higher in soils receiving cattle manure than in soils receiving the other treatments. Increasing cattle manure rates increased fecal coliform population, but there was no indication that increased hog manure rates increased fecal coliform populations. Addition of urea, hog manure, or cattle manure to the soil did not increase foliar disease in wheat, barley, and canola and had variable effects on root rot incidence in cereals.Key words: soil microbial activity, soil microbial populations, microbial community, plant disease, hog manure, cattle manure, urea.
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Dissertations / Theses on the topic "Soils Soils Soil microbiology"

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Jenkins, Anthony Blaine. "Organic carbon and fertility of forest soils on the Allegheny Plateau of West Virginia." Morgantown, W. Va. : [West Virginia University Libraries], 2002. http://etd.wvu.edu/templates/showETD.cfm?recnum=2486.

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Thesis (M.S.)--West Virginia University, 2002.
Title from document title page. Document formatted into pages; contains x, 282 p. : ill. (some col.). Vita. Includes abstract. Includes bibliographical references.
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Hoyle, Frances Carmen. "The effect of soluble organic carbon substrates, and environmental modulators on soil microbial function and diversity /." Connect to this title, 2006. http://theses.library.uwa.edu.au/adt-WU2007.0050.

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Coyle, Kieran. "An investigation of the role of soil micro-organisms in phosphorus mobilisation : a report submitted to fulfil the requrements of the degree of Doctor of Philosophy." Title page, table of contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09PH/09phc8814.pdf.

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Wagai, Rota. "Climatic and Lithogenic Controls on Soil Organic Matter-Mineral Associations." Fogler Library, University of Maine, 2005. http://www.library.umaine.edu/theses/pdf/WagaiR2005.pdf.

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Watts, Dexter Brown. "Mineralization in soils amended with manure as affected by environmental conditions." Auburn, Ala. :, 2007. http://repo.lib.auburn.edu/2007%20Spring%20Dissertations/WATTS_DEXTER_20.pdf.

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Menefee, Dorothy. "Anthropogenic influences on soil microbial properties." Thesis, Kansas State University, 2016. http://hdl.handle.net/2097/32657.

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Master of Science
Department of Agronomy
Ganga M. Hettiarachchi
Human activities have the potential to alter soil biochemical properties in a number of different ways. This thesis will focus on how agricultural practices (tillage and cropping system), climate change, and urban soil pollution (primarily lead and arsenic) affect soil biochemical properties. Two incubation studies were conducted to determine how human activities influence soil biochemical properties. The first study focused on how altered temperature and moisture regimes affected soil properties from four different agroecosystems. Four different soils were incubated under two different soil preparation methods (sieved <4mm and <0.25 mm), three different temperature treatments (12, 24, and 36°C), and two different moisture treatments (field capacity and 80% of field capacity) for 180 days. Destructive samples were taken at 7, 30, 60, 120, and 180 days and the soil microbial community was analyzed using phospholipid fatty acid analysis (PLFA). The second study investigated how soil amendment treatments (Mushroom Compost and Composted Biosolids) of an industrially contaminated site affected the biochemical properties of that soil. Surface soil samples collected 435 days after compost addition from urban garden test plots located adjacent to a former rail yard in Monon, Indiana. Soils were incubated for 30 days to stimulate microbial activity. Following incubation, the soil was analyzed for PLFA, soil enzymes, and available metal fractions. In the first study the greatest differences were found between the <4mm and the <0.25 mm size fractions – which highlights the effect of soil aggregation and structure on microbial populations. After aggregation effects, temperature treatment had the next largest effect on microbial populations, with the greatest biomass in the middle (24°C) treatment. The second study assessed different soil amendments on soil microbial properties and metal availability. Composted biosolids reduced metal availability and increased microbial enzyme activity and biomass.
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Sutanto, Yovita. "Manure from grazing cattle effects on soil microbial communities and soil quality in northern West Virginia pastures /." Morgantown, W. Va. : [West Virginia University Libraries], 2005. https://etd.wvu.edu/etd/controller.jsp?moduleName=documentdata&jsp%5FetdId=3933.

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Thesis (M.S.)--West Virginia University, 2005.
Title from document title page. Document formatted into pages; contains vii, 72 p. : ill. (some col.), map. Includes abstract. Includes bibliographical references.
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Lanza, G. R., and Phillip R. Scheuerman. "Effect of Soil Amendments on In Situ Biodegradation in Creosote Contaminated Soils." Digital Commons @ East Tennessee State University, 1996. https://dc.etsu.edu/etsu-works/2910.

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Padua, Roberto R. "Purification and characterization of an antimicrobial compound secreted by a soil bacterium /." Abstract Full Text (HTML) Full Text (PDF), 2008. http://eprints.ccsu.edu/archive/00000530/02/1979FT.htm.

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Thesis (M.A.) -- Central Connecticut State University, 2008.
Thesis advisor: Michael A. Davis. "... in partial fulfillment of the requirements for the degree of Master of Arts in Biomolecular Sciences." Includes bibliographical references (leaves 36-39). Also available via the World Wide Web.
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Au, William R. "Relationships between microbial physiological status and nitrogen availability in forest soils." Thesis, McGill University, 1998. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=21506.

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Although the physiological nitrogen demand of the soil microbial biomass is a major determinant of N mineralization in forest soils, the exact nature of the relationship is unclear. This study investigated the relationships between a respiration-based indicator of microbial physiological N demand (NIR) and N availability in forest soils. NIR was found to correlate significantly with net mineralized N in the field and annual foliar litterfall N fluxes. In a laboratory incubation, NIR was shown to be sensitive to changes in soil available C and N pools. These results demonstrated that microbial physiological N demand is determined by relative availabilities of labile C and N, and that it is significantly related to N cycling in forest soils. Results from a seasonal study of a forested watershed suggest that nutrient availability determined tree production and soil C availability, which in turn determined microbial physiological N demand and nitrogen dynamics in the forest.
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Books on the topic "Soils Soils Soil microbiology"

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Sorokin, N. D. Mikrobiologicheskai︠a︡ diagnostika lesorastitelʹnogo sostoi︠a︡nii︠a︡ pochv Sredneĭ Sibiri. Novosibirsk: Izd-vo SO RAN, 2009.

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Mikrobnai͡a transformat͡sii͡a organicheskogo veshchestva v lesnykh pochvakh Karelii. Sankt-Peterburg: "Nauka", 1993.

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Omics in soil science. Norfolk, UK: Caister Academic Press, 2014.

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Huang, P. M., and Jianming Xu. Molecular environmental soil science at the interfaces of the earth's critical zone. Heidelberg: Springer, 2010.

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N, Mishustin E., ed. Mikroflora tundrovykh pochv: Ėkologo-geograficheskie osobennosti i produktivnostʹ. Leningrad: "Nauka," Leningradskoe otd-nie, 1989.

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Zakharikhina, L. V. Geneticheskie i geokhimicheskie osobennosti pochv Kamchatki. Moskva: Nauka, 2011.

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Pomazkina, L. V. Biogeokhimicheskiĭ monitoring i ot︠s︡enka rezhimov funkt︠s︡ionirovanii︠a︡ agroėkosistem na tekhnogenno zagri︠a︡zni︠a︡emykh pochvakh. Novosibirsk: Nauka, 1999.

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Sjöqvist, Tore. Soil biochemical and microbial activities as affected by heavy metals and liming. Uppsala: Swedish University of Agricultural Sciences, Dept. of Chemistry, 1995.

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Dion, Patrice, and Chandra Shekhar Nautiyal, eds. Microbiology of Extreme Soils. Berlin, Heidelberg: Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-74231-9.

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Pacific Northwest Forest and Rangeland Soil Organism Symposium (1998 Corvallis, Or.). Proceedings, Pacific Northwest Forest & Rangeland Soil Organism Symposium: Organism functions and processes, management effects on organisms and processes, and role of soil organisms in restoration : LaSells Stewart Center, Oregon State University, Corvallis, Oregon, March 17-19, 1998. Edited by Meurisse Robert T, Ypsilantis William G, Seybold Cathy, and Pacific Northwest Research Station (Portland, Or.). Portland, Or: U.S. Dept. of Agriculture, Forest Service, Pacific Northwest Research Station, 1999.

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Book chapters on the topic "Soils Soils Soil microbiology"

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Ferjani, Eman Ali, Merfat Taher Ben Mahmoud, and Asma Yousef Alnajjar. "Soil Microbiology and Biotechnology." In World Soils Book Series, 91–118. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-66368-1_7.

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Balser, Teri C., Devin Wixon, Lindsey K. Moritz, and Laura Lipps. "The Microbiology of Natural Soils." In Soil Microbiology and Sustainable Crop Production, 27–57. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9479-7_2.

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Gamalero, Elisa, and Bernard R. Glick. "Plant Growth-Promoting Bacteria in Agricultural and Stressed Soils." In Modern Soil Microbiology, 361–80. Third edition. | Boca Raton : Taylor & Francis, 2019.: CRC Press, 2019. http://dx.doi.org/10.1201/9780429059186-22.

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Doelman, P. "Microbiology of Soil and Sediments." In Biogeodynamics of Pollutants in Soils and Sediments, 31–52. Berlin, Heidelberg: Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-79418-6_2.

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Zawar-Reza, Peyman, and Marwan Katurji. "Antarctic Climate and Soils." In Antarctic Terrestrial Microbiology, 279–92. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-45213-0_15.

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Storey, Bryan C. "Origins of Antarctic Soils." In Antarctic Terrestrial Microbiology, 317–28. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-45213-0_17.

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Arenz, Brett E., Robert A. Blanchette, and Roberta L. Farrell. "Fungal Diversity in Antarctic Soils." In Antarctic Terrestrial Microbiology, 35–53. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-45213-0_3.

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Radwan, Samir. "Microbiology of Oil-Contaminated Desert Soils and Coastal Areas in the Arabian Gulf Region." In Soil Biology, 275–98. Berlin, Heidelberg: Springer Berlin Heidelberg, 2008. http://dx.doi.org/10.1007/978-3-540-74231-9_13.

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Bottos, Eric M., Joshua W. Scarrow, Stephen D. J. Archer, Ian R. McDonald, and S. Craig Cary. "Bacterial Community Structures of Antarctic Soils." In Antarctic Terrestrial Microbiology, 9–33. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-45213-0_2.

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Sommers, L. E., C. M. Gilmour, R. E. Wildung, and S. M. Beck. "The Effect of Water Potential on Decomposition Processes in Soils." In Water Potential Relations in Soil Microbiology, 97–117. Madison, WI, USA: Soil Science Society of America, 2015. http://dx.doi.org/10.2136/sssaspecpub9.c3.

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Conference papers on the topic "Soils Soils Soil microbiology"

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Moiseeva, Elena, Aleksandr Khudokormov, Nikita Volchenko, Andrey Samkov, and Maria Kruglova. "The effect of lipids on the natural biodiversity of cultivated aboriginal microflora of urban soils." In 1st International Electronic Conference on Microbiology. Basel, Switzerland: MDPI, 2020. http://dx.doi.org/10.3390/ecm2020-07142.

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Bonilla, N., F. M. Cazorla, J. M. Hermoso, J. González, J. A. Torés, and A. de Vicente. "Microbial analysis of soils from avocado crop modified by organic amendments." In Proceedings of the III International Conference on Environmental, Industrial and Applied Microbiology (BioMicroWorld2009). WORLD SCIENTIFIC, 2010. http://dx.doi.org/10.1142/9789814322119_0016.

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Simpson, R. M., M. Picquet, and M. Deurer. "Differences between microbial communities in worm guts and the soils they inhabit." In Proceedings of the III International Conference on Environmental, Industrial and Applied Microbiology (BioMicroWorld2009). WORLD SCIENTIFIC, 2010. http://dx.doi.org/10.1142/9789814322119_0008.

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Hall, J., R. Stewart, B. Dearman, and A. S. Ball. "Sustainable remediation of polycylic aromatic hydrocarbon contaminated soils using a two-step bioremediation process." In Proceedings of the III International Conference on Environmental, Industrial and Applied Microbiology (BioMicroWorld2009). WORLD SCIENTIFIC, 2010. http://dx.doi.org/10.1142/9789814322119_0055.

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Limane, B., J. Juhanson, J. Truu, M. Truu, O. Muter, A. Versilovskis, L. Dubova, and Dz Zarina. "Changes in microbial population affected by physico-chemical conditions of soils contaminated by explosives." In Proceedings of the II International Conference on Environmental, Industrial and Applied Microbiology (BioMicroWorld2007). WORLD SCIENTIFIC, 2009. http://dx.doi.org/10.1142/9789812837554_0132.

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Caredda, P., A. Franzetti, M. Papacchini, P. La Colla, C. Ruggeri, E. Tamburini, and G. Bestetti. "Applications of Surface Active Compounds by Gordonia in bioremediation and washing of hydrocarbon-contaminated soils." In Proceedings of the II International Conference on Environmental, Industrial and Applied Microbiology (BioMicroWorld2007). WORLD SCIENTIFIC, 2009. http://dx.doi.org/10.1142/9789812837554_0139.

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Gras, A., J. C. Cañadas, and M. Ginovart. "INDISIM-SOM: an individual-based simulator on a website for experimenting with and investigating diverse dynamics of carbon and nitrogen in mineral soils." In Proceedings of the III International Conference on Environmental, Industrial and Applied Microbiology (BioMicroWorld2009). WORLD SCIENTIFIC, 2010. http://dx.doi.org/10.1142/9789814322119_0037.

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Muñoz, Ana, Antonio López-Piñeiro, José A. Regodón, and Manuel Ramírez. "Soil bioremediation of atrazine pesticide by two strains of soil microorganism." In Proceedings of the III International Conference on Environmental, Industrial and Applied Microbiology (BioMicroWorld2009). WORLD SCIENTIFIC, 2010. http://dx.doi.org/10.1142/9789814322119_0029.

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Kokusho, Takaji. "Revisit to Liquefaction of Gravelly Soils Compared with Sandy Soils." In Geotechnical Earthquake Engineering and Soil Dynamics V. Reston, VA: American Society of Civil Engineers, 2018. http://dx.doi.org/10.1061/9780784481455.051.

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Dubova, L., V. Šteinberga, O. Mutere, I. Jansone, and I. Alsiņa. "Influence of organic and conventional soil management system on soil respiration and enzymatic activity." In Proceedings of the III International Conference on Environmental, Industrial and Applied Microbiology (BioMicroWorld2009). WORLD SCIENTIFIC, 2010. http://dx.doi.org/10.1142/9789814322119_0015.

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Reports on the topic "Soils Soils Soil microbiology"

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Carlson, Jake. Agronomy / Soil Microbiology - Purdue University. Purdue University Libraries, September 2011. http://dx.doi.org/10.5703/1288284314994.

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Ponder, Felix Jr, and Darrell E. Alley. Soil sampler for rocky soils. St. Paul, MN: U.S. Department of Agriculture, Forest Service, North Central Research Station, 1997. http://dx.doi.org/10.2737/nc-rn-371.

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Gombert, D. II. Evaluation of soil washing for radiologically contaminated soils. Office of Scientific and Technical Information (OSTI), March 1994. http://dx.doi.org/10.2172/10163686.

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Cunnane, J. C., V. R. Gill, S. Y. Lee, D. E. Morris, M. D. Nickelson, D. L. Perry, and V. C. Tidwell. Uranium soils integrated demonstration: Soil characterization project report. Office of Scientific and Technical Information (OSTI), August 1993. http://dx.doi.org/10.2172/10180428.

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Duncan, David Sean. Linking soil microbiology and environmental conditions to variability in nitrous oxide production in bioenergy cropping systems. Office of Scientific and Technical Information (OSTI), July 2016. http://dx.doi.org/10.2172/1477790.

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Drumm, E. C. Soil mechanics and analysis of soils overlying cavitose bedrock. Office of Scientific and Technical Information (OSTI), August 1987. http://dx.doi.org/10.2172/5998770.

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Drnevich, Vincent, Aaron Evans, and Adam Prochaska. A Study of Effective Soil Compaction Control of Granular Soils. West Lafayette, IN: Purdue University, 2007. http://dx.doi.org/10.5703/1288284313357.

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Brandt, C. A., K. Alford, G. McIlveny, and A. Tijerina. Plant reestablishment after soil disturbance: Effects of soils, treatment, and time. Office of Scientific and Technical Information (OSTI), November 1993. http://dx.doi.org/10.2172/10106314.

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Hazard, John W., Jeralyn Snellgrove, and J. Michael Geist. Processing data from soil assessment surveys with the computer program SOILS. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Forest and Range Experiment Station, 1985. http://dx.doi.org/10.2737/pnw-gtr-179.

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Acton, D. F. Soils As a Resource: Soil Formation [Chapter 11: Quaternary Resources in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131666.

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