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Artículos de revistas sobre el tema "Soil biology"

Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 9 de junio de 2025

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1

Holt, John. "Soil biology." Geoderma 53, no. 1-2 (May 1992): 173–74. http://dx.doi.org/10.1016/0016-7061(92)90032-3.

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2

Tate, Robert L. "Soil Biology. 1989." Soil Science 150, no. 5 (November 1990): 828. http://dx.doi.org/10.1097/00010694-199011000-00009.

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3

Valentine, Barry D. "Soil Biology Guide." American Entomologist 38, no. 3 (1992): 181–82. http://dx.doi.org/10.1093/ae/38.3.181a.

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4

New, T. R. "Soil biology guide." Soil Biology and Biochemistry 23, no. 7 (January 1991): 707–8. http://dx.doi.org/10.1016/0038-0717(91)90088-2.

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5

Lehman, R. M., V. Acosta-Martinez, J. S. Buyer, C. A. Cambardella, H. P. Collins, T. F. Ducey, J. J. Halvorson, et al. "Soil biology for resilient, healthy soil." Journal of Soil and Water Conservation 70, no. 1 (January 1, 2015): 12A—18A. http://dx.doi.org/10.2489/jswc.70.1.12a.

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6

Coleman, D. C., E. P. Odum, and D. A. Crossley. "Soil biology, soil ecology, and global change." Biology and Fertility of Soils 14, no. 2 (October 1992): 104–11. http://dx.doi.org/10.1007/bf00336258.

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7

Robinson, Clare, F. Schinner, R. Ohlinger, E. Kandeler, and R. Margesin. "Methods in Soil Biology." Journal of Ecology 85, no. 3 (June 1997): 404. http://dx.doi.org/10.2307/2960521.

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8

Edwards, Clive A. "Soil Biology. Tertiary Level Biology. Martin Wood." Quarterly Review of Biology 66, no. 2 (June 1991): 224. http://dx.doi.org/10.1086/417204.

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9

Mantoni, Cristina, Marika Pellegrini, Leonardo Dapporto, Maria Del Gallo, Loretta Pace, Donato Silveri, and Simone Fattorini. "Comparison of Soil Biology Quality in Organically and Conventionally Managed Agro-Ecosystems Using Microarthropods." Agriculture 11, no. 10 (October 19, 2021): 1022. http://dx.doi.org/10.3390/agriculture11101022.

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Since management practices profoundly influence soil characteristics, the adoption of sustainable agro-ecological practices is essential for soil health conservation. We compared soil health in organic and conventional fields in the Abruzzi region (central Italy) by using (1) the soil biology quality (QBS) index (which expresses the level of specialisation in soil environment shown by microarthropods) and (2) microarthropod diversity expressed by Hill numbers. QBS values were calculated using both the original formulation based on only presence/absence data and a new abundance-based version. We found that organic management improves soil biology quality, which encourages the use of organic farming to maintain soil health. Including arthropod abundance in QBS calculation does not change the main outcomes, which supports the use of its original, speedier formulation. We also found that agricultural fields included in protected areas had greater soil health, which shows the importance of the matrix in determining agricultural soil health and highlights the importance of land protection in preserving biodiversity even in managed soils. Finally, we found that soil biology quality and microarthropod community structure are distinctly influenced by certain physical and chemical characteristics of the soil, which supports the use of microarthropods as biological indicators.

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10

Lussenhop, John. "Soil Biology for Ecological Students." Ecology 71, no. 6 (December 1990): 2399. http://dx.doi.org/10.2307/1938658.

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11

Usher, M. B., P. Lebrun, H. M. Andre, A. De Medts, C. Gregoire-Wibo, and G. Wauthy. "New Trends in Soil Biology." Journal of Animal Ecology 54, no. 1 (February 1985): 337. http://dx.doi.org/10.2307/4644.

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12

Lynch, J. M. "Soil Biology: Accomplishments and Potential." Soil Science Society of America Journal 51, no. 6 (November 1987): 1409–12. http://dx.doi.org/10.2136/sssaj1987.03615995005100060004x.

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13

Mitchell, Myron J. "Soil Biology Guide.Daniel L. Dindal." Quarterly Review of Biology 66, no. 1 (March 1991): 101–2. http://dx.doi.org/10.1086/417109.

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14

Anderson, J. M., and J. S. I. Ingram. "Tropical Soil Biology and Fertility." Soil Science 157, no. 4 (April 1994): 265. http://dx.doi.org/10.1097/00010694-199404000-00012.

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15

Ohtonen, R., S. Aikio, and H. Väre. "Ecological theories in soil biology." Soil Biology and Biochemistry 29, no. 11-12 (November 1997): 1613–19. http://dx.doi.org/10.1016/s0038-0717(97)00063-1.

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16

Geisen, Stefan, Edward A. D. Mitchell, Sina Adl, Michael Bonkowski, Micah Dunthorn, Flemming Ekelund, Leonardo D. Fernández, et al. "Soil protists: a fertile frontier in soil biology research." FEMS Microbiology Reviews 42, no. 3 (February 13, 2018): 293–323. http://dx.doi.org/10.1093/femsre/fuy006.

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17

POP, Bianca, Roxana VIDICAN, and Camelia MUNTEANU. "The Effects of Heavy Metals on Soil Biology." Bulletin of University of Agricultural Sciences and Veterinary Medicine Cluj-Napoca. Agriculture 80, no. 1 (May 15, 2023): 8–16. http://dx.doi.org/10.15835/buasvmcn-agr:2022.0019.

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Heavy metal pollution is a global environmental issue threatening food security and the environment. It is caused by the rapid growth of agriculture and industry. The development of new industries and the increasing number of people have also contributed to the rise in these conditions. Heavy metals that contaminate soils are mercury (Hg), cadmium (Cd), lead (Pb), and chromium (Cr), these toxic substances are retained by the soil and act as a filter for their properties. The aim of this paper was to review the impact of heavy metals on soil, as well as the methods to combat their toxicity in agricultural ones. In order to achieve this goal, data belonging to national and international databases were used (Science Direct, NCBI). The finding of different strategies to combat pollution, particularly on the soil represented the goals for the majority of the studies. As such, bioremediation is a promising choice to reduce heavy metal concentrations.

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18

Romanova, Tatyana, Aliaksandr Chervan, and Nadezhda Ivakhnenko. "The essence of soil and soil formation in accordance with soil water regime." Journal of Geography and Cartography 7, no. 2 (November 4, 2024): 6271. http://dx.doi.org/10.24294/jgc.v7i2.6271.

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The obtaining of new data on the transformation of parent materials into soil and on soil as a set of essential properties is provided on the basis of previously conducted fundamental studies of soils formed on loess-like loams in Belarus (15,000 numerical indicators). The study objects are autochthonous soils of uniform granulometric texture. The basic properties without which soils cannot exist are comprehensively considered. Interpolation of factual materials is given, highlighting the essential properties of soils. Soil formation is analyzed as a natural phenomenon depending on the life activity of biota and the water regime. Models for differentiation of the chemical profile and bioenergy potential of soils are presented. The results of the represented study interpret the available materials taking into account publications on the biology and water regime of soils over the past 50 years into three issues: the difference between soil and soil-like bodies; the soil formation as a natural phenomenon of the mobilization of soil biota from the energy of the sun, the atmosphere, and the destruction of minerals in the parent materials; and the essence of soil as a solid phase and as an ecosystem. The novelty of the article study is determined by the consideration of the priority of microorganisms and water regime in soil formation, chemical-analytical identification of types of water regime, and determination of the water regime as a marker of soil genesis.

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19

Coyne, M. S., E. M. Pena-Yewtukhiw, J. H. Grove, A. C. Sant'Anna, and D. Mata-Padrino. "Soil health – It's not all biology." Soil Security 6 (March 2022): 100051. http://dx.doi.org/10.1016/j.soisec.2022.100051.

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20

Burns, R. "Soil Biology & Biochemistry Citation Classics." Soil Biology and Biochemistry 36, no. 1 (January 2004): 3. http://dx.doi.org/10.1016/j.soilbio.2003.10.001.

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21

Briggs, Winslow R. "Plant Biology: Seedling Emergence through Soil." Current Biology 26, no. 2 (January 2016): R68—R70. http://dx.doi.org/10.1016/j.cub.2015.12.003.

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22

Rao, D. L. N. "Experiments in soil biology and biochemistry." Indian Journal of Microbiology 47, no. 2 (June 2007): 184. http://dx.doi.org/10.1007/s12088-007-0037-3.

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23

O’DONOVAN, J. T., and M. P. SHARMA. "THE BIOLOGY OF CANADIAN WEEDS.: 78. Galeopsis tetrahit L." Canadian Journal of Plant Science 67, no. 3 (July 1, 1987): 787–96. http://dx.doi.org/10.4141/cjps87-106.

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Galeopsis tetrahit is an annual weed which was introduced to North America from Eurasia. It is present in all Canadian provinces and occupies a wide range of habitats including cultivated fields. It favors well-watered nutrient-rich soils and occurs infrequently in the drier brown soil zones of the southern Canadian prairies. Low soil moisture may be a major factor limiting its distribution and spread. It can reduce crop yields, contaminate crop seed and act as a reservoir for disease-causing organisms. A number of herbicides are available for its control.Key words: Hemp-nettle, Galeopsis tetrahit L., weed ecology, weed biology

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24

Vilkova, Valeria, Kamil Kazeev, Aslan Shkhapatsev, Mikhail Nizhelsky, and Sergey Kolesnikov. "Pyrogenic impact on biology activity of chernozem in model experiments." АгроЭкоИнфо 5, no. 47 (October 24, 2021): 20. http://dx.doi.org/10.51419/20215520.

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The influence of the pyrogenic effect on the biological properties of Haplic chernozem was investigated. For this, a series of model experiments was set up to simulate fires of various duration and intensity. A significant change in the biological properties of soils was found, as well as differences in the reactions of biological indicators to the pyrogenic effect. In different experiments, a different nature of changes in the reaction of the soil environment and the content of organic carbon, an increase in the content of readily soluble salts, was established. In all experiments, inhibition of catalase activity was noted, changes in peroxidase activity were more contradictory. In one of the experiments, stimulation of peroxidase activity was found. In order to study the methods of restoring the biological activity of post-pyrogenic soils, a model experiment was carried out using potassium humate, complex mineral fertilizer and phytoremediation. At the same time, no unambiguous results were obtained that would make it possible to recommend methods for the accelerated recovery of post-pyrogenic soils. Keywords: BIODIAGNOSTICS, FIRES, POSTPYROGENIC SOILS, ENZYME ACTIVITY, SOIL RESTORATION

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25

Bhunia, Shantanu, Ankita Bhowmik, Rambilash Mallick, and Joydeep Mukherjee. "Agronomic Efficiency of Animal-Derived Organic Fertilizers and Their Effects on Biology and Fertility of Soil: A Review." Agronomy 11, no. 5 (April 22, 2021): 823. http://dx.doi.org/10.3390/agronomy11050823.

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Healthy soils are essential for progressive agronomic activities. Organic fertilization positively affects agro-ecosystems by stimulating plant growth, enhancing crop productivity and fruit quality and improving soil fertility. Soil health and food security are the key elements of Organic Agriculture 3.0. Landfilling and/or open-dumping of animal wastes produced from slaughtering cause environmental pollution by releasing toxic substances, leachate and greenhouse gases. Direct application of animal carcasses to agricultural fields can adversely affect soil microbiota. Effective waste management technologies such as thermal drying, composting, vermicomposting and anaerobic digestion transform animal wastes, making them suitable for soil application by supplying soil high in organic carbon and total nitrogen. Recent agronomic practices applied recycled animal wastes as organic fertilizer in crop production. However, plants may not survive at a high fertilization rate due to the presence of labile carbon fraction in animal wastes. Therefore, dose calculation and determination of fertilizer application frequency are crucial for agronomists. Long-term animal waste-derived organic supplementation promotes copiotrophic microbial abundance due to enhanced substrate affinity, provides micronutrients to soils and protects crops from soil-borne pathogens owing to formation of plant-beneficial microbial consortia. Animal waste-derived organically fertilized soils possess higher urease and acid phosphatase activities. Furthermore, waste to fertilizer conversion is a low-energy requiring process that promotes circular bio-economy. Thus, considering the promotion of soil fertility, microbial abundance, disease protection and economic considerations application of animal-waste-derived organic fertilizer should be the mainstay for sustainable agriculture.

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26

Forge, T., G. Neilsen, D. Neilsen, D. O'Gorman, E. Hogue, and D. Angers. "ORGANIC ORCHARD SOIL MANAGEMENT PRACTICES AFFECT SOIL BIOLOGY AND ORGANIC MATTER." Acta Horticulturae, no. 1076 (March 2015): 77–84. http://dx.doi.org/10.17660/actahortic.2015.1076.8.

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27

Bölter, Manfred. "Soil development and soil biology on King George Island, Maritime Antarctic." Polish Polar Research 32, no. 2 (January 1, 2011): 105–16. http://dx.doi.org/10.2478/v10183-011-0002-z.

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Soil development and soil biology on King George Island, Maritime AntarcticThis review covers aspects of soil science and soil biology of Antarctica with special focus on King George Island, South Shetlands, the martitime Antarctic. New approaches in soil descriptions and soil taxonomy show a great variety of soil types, related to different parent material, mainly volcanic origin, as well as on influences by soil biological processes. The spread of higher rooting plants attract microorganisms, nematodes and collemboles which in turn build new organic material and change the environment for further successors. Microbial communities are drivers with respect to metabolic and physiological properties indicating a great potential in a changing environment. The literature review also shows a lack of investigations on processes of carbon and nitrogen turnover, despite wide knowledge on its standing stock in different environments. Further, only few reports were found on the processes of humification. Only few data are available which can be regarded as long term monitorings, hence, such projects need to be established in order to follow ecological changes.

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28

Wong, J. W. C., K. M. Lai, M. Fang, and K. K. Ma. "Soil Biology of Low Grade Landfill Soil with Sewage Sludge Amendment." Environmental Technology 21, no. 11 (November 2000): 1233–38. http://dx.doi.org/10.1080/09593332108618149.

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29

Hüberli, Daniel. "Soil health, soil biology, soilborne diseases and sustainable agriculture: A guide." Australasian Plant Pathology 46, no. 4 (May 19, 2017): 387. http://dx.doi.org/10.1007/s13313-017-0493-0.

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30

STEPANOV, A. L., N. A. MANUCHAROVA, D. A. NIKITIN, and M. V. SEMENOV. "ACHIEVEMENTS AND PERSPECTIVES OF DEVELOPMENT IN SOIL MICROBIOLOGY AT MOSCOW UNIVERSITY." Ser-17_2023-4 78, no. 4, 2023 (December 16, 2023): 63–69. http://dx.doi.org/10.55959/msu0137-0944-17-2023-78-4-63-69.

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The article summarizes the results of recent research by the staff of Soil Biology Department Faculty of Soil Science of Lomonosov Moscow State University in the field of assessing the genetic potential of microbial communities of soils and their application in the development of fundamental soil and environmental technologies. Promising areas of further work related to the use of the microbial potential of soils for the purpose of bioremediation territories from ecotoxicants, the development of technologies for selfpurification of soils based on the stimulation of natural communities of microorganisms, as well as the use of microbial cultures for biodegradation of petroleum products, pesticides and synthetic polymers. Another important direction is related to the development of scientific basis for the indication of biological objects in the environment and space objects. Within the framework of this direction, genomic analysis of uncultivated microorganisms from the Arctic, Antarctic and other extreme habitats is carried out, and the knowledge gained apply as a model of alien life. Another relevant direction for the Department of Soil Biology is the development of agrobiotechnologies based on the management of the natural soil microbiome, the creation of microbial preparationsstimulators of plant growth and development, microbiological ways to increase the proportion of biological nitrogen in plant nutrition, application of microbial plant endosymbionts and bioinsecticides. An equally important aspect is the search of producers of biologically active substances, such as phytohormones, antibiotics, enzymes, probiotics, hydrolytics of natural and artificial polymers. The considered areas of research in the field of soil biology are important for improving land management, environmental protection and the development of environmental technologies.

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31

ARTHAGAMA, I. DEWA MADE, and I. MADE DANA. "Evaluasi Kualitas Tanah Sawah Intensif dan Sawah yang Dikonversikan untuk Kebun di Subak Kesiut Kerambitan Tabanan." Agrotrop : Journal on Agriculture Science 10, no. 1 (May 29, 2020): 1. http://dx.doi.org/10.24843/ajoas.2020.v10.i01.p01.

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Evaluation Quality of Intensif Paddy Soils and Conversion Paddy Soils to Garden at Subak Kesiut Kerambitan Tabanan. This experiment conducted to evaluate intensif Paddy Soils and conversion paddy soils to garden at SubakKesiut Kerambitan Tabanan. There were two steps applied in this study including field survey to determine the research area and points soils sampling; analysis soils properties are: physic, chemistry and soils biology for get minimum data set to determine the soil quality at Laboratory of Soils and Enveronment Faculty of Agriculture Unud. The results of this study showed: the soil quality of intensif paddy soils is better than conversion paddy soils to garden, that showed with SQR at intensif paddy soil is 18 and at conversions paddy soil is 25. The limiting faktor at conversion paddy soils to garden is P available, there are less than at intensif paddy soils.

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32

Sabirova, Razina, Il'shat Vafin, Arina Abramova, and Radik Safin. "COMPREHENSIVE ASSESSMENT OF SOIL CONDITION AFTER VARIOUS CROPS." Agrobiotechnologies and digital farming 1, no. 4 (December 28, 2022): 40–44. http://dx.doi.org/10.12737/2782-490x-2022-40-44.

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The paper presents an assessment of the state of the soil after harvesting crops (cereals, legumes, technical, perennial grasses) on the experimental fields of the Agrobiotechnopark of Kazan State Agrarian University in industrial crops. The studies were carried out in 2022, which was characterized by significant differences in moisture conditions during the growing season of plants (the first half of the growing season is wet, the second half is dry). All plots were located on highly cultivated, gray forest, medium loamy soil. A comprehensive assessment of soils was carried out using the methods of agrophysical studies of soils and methods of soil biology. To assess the state of soil biology, the number of microorganisms, Protozoa and nematodes was taken into account. Simultaneously, the phytotoxicity of soils for model plants was determined. Analysis of the accumulation of available water in the soil and the share of agronomically valuable aggregates showed that the maximum values were after mustard. After this crop, there was a decrease in the density of soil composition. The deterioration of the agrophysical properties of the soil was noted after spring crops. A pronounced phytotoxic effect of soil extracts after spring barley, peas and potatoes was established in relation to lettuce test plants. A similar effect on the wheat test plant was noted after potatoes. Improvement in agrophysical properties, low phytotoxicity and suppression of the development of Fusarium fungi among the studied crops, the advantage was noted for Sarepta mustard. After peas, an increase in the number of Azotobacter bacteria in the soil was noted, and after winter wheat, an increase in the number of ciliates in the soil was noted. The results obtained confirmed the differences in the state of soils after various crops, which must be taken into account when selecting predecessors in crop rotation.

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33

Blagodatsky, Sergey, and Pete Smith. "Soil physics meets soil biology: Towards better mechanistic prediction of greenhouse gas emissions from soil." Soil Biology and Biochemistry 47 (April 2012): 78–92. http://dx.doi.org/10.1016/j.soilbio.2011.12.015.

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34

Read, D. J., and R. Bajwa. "Some nutritional aspects of the biology of ericaceous mycorrhizas." Proceedings of the Royal Society of Edinburgh. Section B. Biological Sciences 85, no. 3-4 (1985): 317–31. http://dx.doi.org/10.1017/s0269727000004097.

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SynopsisSome aspects of the role of the ericoid mycorrhizal symbiosis in the ecology and physiology of ericaceous plants are described. Mycorrhizal infection leads to enhancement of plant nitrogen content and an experimental analysis of the basis of this effect is reported. In addition to improving the efficiency of ammonium absorption at low concentrations, the mycorrhizal endophyte utilises amino acids, peptides and proteins as nitrogen substrates for growth. These are the predominant nitrogen sources in organic heathland soil. It is suggested that the success of ericaceous plants in such soils may arise through the capacity of the mycorrhizal fungus to provide its host with access to this nutrient resource. A model is described in which absorption of ammonium and amino nitrogen leads to soil acidification, increased acid protease activity and improved vigour of the ericaceous plants.

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35

Wyatt, Briana, and Susan Chapman. "Soil Biology, Chemistry, and Physics … Oh My!" CSA News 66, no. 6 (May 30, 2021): 44. http://dx.doi.org/10.1002/csan.20485.

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36

Uroz, S., A. Bispo, M. Buee, A. Cebron, J. Cortet, T. Decaens, M. Hedde, G. Peres, M. Vennetier, and C. Villenave. "Highlights on progress in forest soil biology." Revue Forestière Française, SP (2014): Fr.], ISSN 0035. http://dx.doi.org/10.4267/2042/56266.

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37

GC, Sagar, Prakash Banakar, David Harshman, and Churamani Khanal. "Elevated Soil Temperatures Impact Nematode Reproduction Biology." Stresses 5, no. 1 (January 3, 2025): 2. https://doi.org/10.3390/stresses5010002.

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Plant-parasitic nematodes are one of the economically most important pathogens, and how rising soil temperatures due to climate change impact their ability to damage crops is poorly understood. The current study was conducted to evaluate the reproduction biology (reproduction and virulence) of Rotylenchulus reniformis and Meloidogyne floridensis on tomato at soil temperatures of 26 °C (control), 32 °C, 34 °C, and 36 °C. The reproduction and virulence of both nematode species were differentially impacted by soil temperature. Relative to the control, the increase in reproduction of R. reniformis ranged from 20% to 116% while that of M. floridensis ranged from 22% to 133%. The greatest reproduction of R. reniformis was observed at 34 °C while that of M. floridensis was observed at 32 °C. Across all temperatures, reproduction of M. floridensis was 2.9 to 7.8 times greater than the reproduction of R. reniformis, suggesting that the former nematode species has a greater fecundity. The rates of change in reproduction relative to the controls were greater in M. floridensis than in R. reniformis, indicating that the latter nematode species is more resilient to changes in soil temperature. The virulence of both nematode species increased numerically or significantly at 32 °C and 36 °C, but not at 34 °C. The greatest virulence of both nematode species was observed at 36 °C at which 57% and 60% root biomass was lost to R. reniformis and M. floridensis, respectively, compared to the root biomass of uninoculated plants at that temperature. The results of the current study suggested that crop damage by nematodes will likely increase as global soil temperature continues to increase.

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38

Creamer, R. E. "The Biology of Soil - by R.D. Bardgett." European Journal of Soil Science 58, no. 5 (October 2007): 1214. http://dx.doi.org/10.1111/j.1365-2389.2007.00943_2.x.

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39

Andrén, O., H. Kirchmann, T. Kätterer, J. Magid, E. A. Paul, and D. C. Coleman. "Visions of a more precise soil biology." European Journal of Soil Science 59, no. 2 (April 2008): 380–90. http://dx.doi.org/10.1111/j.1365-2389.2008.01018.x.

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40

BURNS, R. "Soil Biology & Biochemistry Citation Classic IV." Soil Biology and Biochemistry 38, no. 9 (September 2006): 2509. http://dx.doi.org/10.1016/j.soilbio.2006.03.001.

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41

Burns, Richard G. "Soil Biology & Biochemistry Citation Classic VI." Soil Biology and Biochemistry 41, no. 10 (October 2009): 2029–30. http://dx.doi.org/10.1016/j.soilbio.2009.07.004.

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42

Burns, Richard G. "Soil Biology & Biochemistry Citation Classic VII." Soil Biology and Biochemistry 42, no. 9 (September 2010): 1361–62. http://dx.doi.org/10.1016/j.soilbio.2010.05.014.

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43

Burns, Richard G. "Soil Biology & Biochemistry Citation Classic VIII." Soil Biology and Biochemistry 42, no. 12 (December 2010): 2037–38. http://dx.doi.org/10.1016/j.soilbio.2010.08.028.

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44

Burns, Richard G. "Soil Biology & Biochemistry Citation Classic IX." Soil Biology and Biochemistry 43, no. 5 (May 2011): 871–72. http://dx.doi.org/10.1016/j.soilbio.2011.01.006.

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45

Burns, Richard G. "Soil Biology & Biochemistry Citation Classic X." Soil Biology and Biochemistry 43, no. 8 (August 2011): 1619–20. http://dx.doi.org/10.1016/j.soilbio.2011.03.021.

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46

Burns, Richard G. "Soil Biology & Biochemistry Citation Classic XI." Soil Biology and Biochemistry 64 (September 2013): 200–202. http://dx.doi.org/10.1016/j.soilbio.2012.09.023.

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Burns, Richard G. "Soil Biology & Biochemistry Citation Classic XII." Soil Biology and Biochemistry 68 (January 2014): A1—A3. http://dx.doi.org/10.1016/j.soilbio.2013.09.003.

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Szegi, J. "Soil Biology and Conservation of the Biosphere." Soil Science 141, no. 3 (March 1986): 245. http://dx.doi.org/10.1097/00010694-198603000-00012.

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Burns, Richard G. "Soil Biology & Biochemistry Citation Classic XIII." Soil Biology and Biochemistry 80 (January 2015): A1—A2. http://dx.doi.org/10.1016/j.soilbio.2014.10.001.

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Burns, Richard G. "Soil Biology & Biochemistry Citation Classic XIV." Soil Biology and Biochemistry 105 (February 2017): A1—A2. http://dx.doi.org/10.1016/j.soilbio.2016.08.012.

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