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Journal articles on the topic 'Soil micromorphology'

Author: Grafiati

Published: 4 June 2021

Last updated: 27 July 2024

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1

Nettleton, W. D. "Micromorphologie des sols - soil micromorphology." Geoderma 48, no. 1-2 (1991): 179. http://dx.doi.org/10.1016/0016-7061(91)90015-l.

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2

Ellis, Clare. "Soil micromorphology." Scottish Archaeological Internet Reports 96 (August 2, 2021): 70–73. http://dx.doi.org/10.9750/issn.2056-7421.2021.96.70-73.

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3

Stoops, George, and Hari Eswaran. "Soil Micromorphology." Soil Science 145, no. 2 (1988): 156. http://dx.doi.org/10.1097/00010694-198802000-00014.

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4

&NA;. "Soil Micromorphology." Soil Science 152, no. 4 (1991): 312. http://dx.doi.org/10.1097/00010694-199110000-00012.

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5

Nortcliff, Stephen. "Soil micromorphology." Progress in Physical Geography: Earth and Environment 9, no. 2 (1985): 281–90. http://dx.doi.org/10.1177/030913338500900204.

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6

Cao, Tingting, Jian Wang, and Haiou Zhang. "The Significance of Soil Micromorphology Research in Land Reclamation." E3S Web of Conferences 338 (2022): 01042. http://dx.doi.org/10.1051/e3sconf/202233801042.

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Soil micromorphology is an emerging branch of soil science that aims to study the formation and structure of soils at a microscopic level. The study of soil micromorphology can be used for the analysis of soil genesis and evolution, the development of land remediation techniques, the analysis of the causes of geological hazards, the mechanisms of soil quality degradation, the process of soil formation and material changes in “anthropogenic soils” and many other aspects. With the gradual development of instrumentation, scanning electron microscopy, light microscopy and scanning CT have been wid

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7

Lebedeva, M. P., I. V. Kovda, M. I. Gerasimova, and E. V. Dostovalova. "Current trends in soil micromorphology: bibliometric approach." Dokuchaev Soil Bulletin 86 (December 15, 2016): 17–27. http://dx.doi.org/10.19047/0136-1694-2016-86-17-27.

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8

DREES, RICHARD. "Soil Microscopy and Micromorphology." Soil Science 158, no. 5 (1994): 382–87. http://dx.doi.org/10.1097/00010694-199411000-00012.

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9

Arocena, J. M. "Soil microscopy and micromorphology." Geoderma 66, no. 1-2 (1995): 155–57. http://dx.doi.org/10.1016/0016-7061(95)90038-1.

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10

He, Yurong, Peng Cui, Chaolin Liao, Baohua Zhang, and Yu Zhao. "Micromorphology of landslide soil." Journal of Mountain Science 3, no. 2 (2006): 147–57. http://dx.doi.org/10.1007/s11629-006-0147-0.

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11

Thompson, Michael L. "Soil microscopy and micromorphology." Geochimica et Cosmochimica Acta 58, no. 18 (1994): 3971–72. http://dx.doi.org/10.1016/0016-7037(94)90374-3.

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12

Macphail, Richard I., Marie-Agnès Courty, and Paul Goldberg. "Soil micromorphology in archaeology." Endeavour 14, no. 4 (1990): 163–71. http://dx.doi.org/10.1016/0160-9327(90)90039-t.

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13

Kodešová, R. "Soil micromorphology use for modeling of a non-equilibrium water and solute movement." Plant, Soil and Environment 55, No. 10 (2009): 424–28. http://dx.doi.org/10.17221/137/2009-pse.

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Soil micromorphology was applied to specify flow domains in different soils and to select a suitable numerical model for simulation of water flow and herbicide transport. Pore structure detected on soil micromorphological images represented in all cases domains of prevailing water flow and solute transport. Depending on pore configuration and boundary conditions either water immobilization or preferential flow was observed and simulated. The benefits and limitations of the soil micromorphology imaging are discussed and compared with the more often used X-ray computer tomography, magnetic reson

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14

Forman, Steven L., and R. A. Kemp. "Soil Micromorphology and the Quaternary." Arctic and Alpine Research 18, no. 4 (1986): 448. http://dx.doi.org/10.2307/1551102.

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15

&NA;. "Soil Micromorphology and the Quaternary." Soil Science 144, no. 5 (1987): 385. http://dx.doi.org/10.1097/00010694-198711000-00012.

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16

Fitz-Patrick, E. A., and MARTIN C. RABENHORST. "Micromorphology of Soils." Soil Science 141, no. 1 (1986): 88. http://dx.doi.org/10.1097/00010694-198601000-00014.

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17

De Coninck, F. "Micromorphology of Soils." Geoderma 37, no. 1 (1986): 67–68. http://dx.doi.org/10.1016/0016-7061(86)90044-3.

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18

Bronnikova, M. A., A. V. Panin, V. V. Murasheva, and A. A. Golyeva. "Soil micromorphology in archaeology: history, objectives, possibilities and prospects." Dokuchaev Soil Bulletin 86 (December 15, 2016): 35–45. http://dx.doi.org/10.19047/0136-1694-2016-86-35-45.

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19

Juhász, Carlos Eduardo Pinto, Miguel Cooper, Patrícia Ribeiro Cursi, André Oppitz Ketzer, and Raul Shiso Toma. "Savanna woodland soil micromorphology related to water retention." Scientia Agricola 64, no. 4 (2007): 344–54. http://dx.doi.org/10.1590/s0103-90162007000400005.

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The limiting factors of the Brazilian savanna physical environment have been largely discussed. Soil morphology is fundamental to understand the behavior of soil water flow, soil physical properties and soil-landscape relationships. The aim of this study is to relate soil micro and macromorphologic attributes to soil water retention on a toposequence under native savanna woodland (cerradão) in a permanent plot of 320 m <FONT FACE=Symbol>´</FONT> 320 m installed in Assis, SP, Brazil. Samples collected at five points within the toposequence were used to determine the soil macroporosi

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20

Karpova, D. V., P. N. Balabko, N. P. Chizhikova, et al. "THE MICROMORPHOLOGY AND MINERALOGY OF GRAY FOREST SOILS IN VLADIMIR OPOLYE." Dokuchaev Soil Bulletin, no. 94 (September 1, 2018): 101–23. http://dx.doi.org/10.19047/0136-1694-2018-94-101-123.

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The investigations were conducted on the gray forest heavy clay loamy soils, formed on the loess-like loams, which are widely spread on the territory of Vladimir Opolye. The eluvial-illuvial profile differentiation, its different intensity and the specificity of illuvial coatings (fine dispersed clayey and humus-clayey coatings with sparse skeletal content of soil) is confirmed. The presence of the coarse wooden plant residues, thick humus-clayey illuvial coatings within the illuvial horizons speak about the forest origin of the grey forest soils in Vladimir Opolye. The micromorphology of humu

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21

Courty, Marie-Agnes, Paul Goldberg, and Richard Macphail. "Soils and Micromorphology in Archaeology." Soil Science 150, no. 6 (1990): 904. http://dx.doi.org/10.1097/00010694-199012000-00014.

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22

Davidson, Donald A. "Bioturbation in Old Arable Soils: Quantitative Evidence from Soil Micromorphology." Journal of Archaeological Science 29, no. 11 (2002): 1247–53. http://dx.doi.org/10.1006/jasc.2001.0755.

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23

Ringrose-Voase, AJ. "Micromorphology of soil structure - Description, quantification, application." Soil Research 29, no. 6 (1991): 777. http://dx.doi.org/10.1071/sr9910777.

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Micromorphological observation can provide insights into soil structure and aid interpretation of soil behaviour. Undisturbed samples are taken in the field and impregnated. They are used to prepare thin sections or images of the macropore structure using fluorescent photography. Sections can also be obtained at macro, meso and submicroscopic scales. The various elements of soil structure observed micromorphologically can be classified into pore space, physical, distribution and orientation fabrics, and associated structures. Examples of the importance of features in each category are given. I

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24

Kemp, R. A. "Soil micromorphology of local authority cricket tables." Soil Use and Management 10, no. 2 (1994): 65–71. http://dx.doi.org/10.1111/j.1475-2743.1994.tb00461.x.

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25

Tursina, T. V. "The 12th international conference on soil micromorphology." Eurasian Soil Science 39, no. 1 (2006): 110–12. http://dx.doi.org/10.1134/s1064229306010157.

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26

Tursina, T. V. "The 13th International Conference on Soil Micromorphology." Eurasian Soil Science 43, no. 1 (2010): 110–13. http://dx.doi.org/10.1134/s106422931001014x.

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27

Bui, Elisabeth N. "Applications of image analysis to soil micromorphology." Agriculture, Ecosystems & Environment 34, no. 1-4 (1991): 305–13. http://dx.doi.org/10.1016/0167-8809(91)90116-f.

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28

Fox, C. A., C. M. Preston, and C. A. Fyfe. "Micromorphological and 13C NMR characterization of a Humic, Lignic, and Histic Folisol from British Columbia." Canadian Journal of Soil Science 74, no. 1 (1994): 1–15. http://dx.doi.org/10.4141/cjss94-001.

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The thick folic (mainly upland forest) materials (> 40 cm of accumulated organic material) that occur in the Coastal Western Hemlock Biogeoclimatic Zone in British Columbia have not been described with regard to the spatial interrelationships of the soil constituents in context with the chemical composition of the different horizons. Micromorphological assessment and solid-state 13C NMR were used to characterize the accumulated folic materials from a Lignic Folisol (northern Vancouver Island), Histic Folisol (Prince Rupert, BC) and a Humic Folisol (Queen Charlotte Islands, BC). Micromorphol

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29

Gus, M., and M. Drewnik. "Evolution of sandy soils within deflation hollows in shifting areas of sand – a case study from the Błędów Desert (Poland)." Soil and Water Research 12, No. 3 (2017): 161–69. http://dx.doi.org/10.17221/36/2016-swr.

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Areas of shifting sand are important places for testing the effects of abiotic and biotic factors on soil morphology and evolution, where aeolian processes cause dynamic changes in the natural environment. The main aim of the study was to determine the evolution of soils within deflation hollows in shifting sands. In the context of this purpose, representative study areas were selected: (1) a reference surface in a plantation forest with soils undisturbed by aeolian processes – one pedon, (2) an active deflation hollow – two pedons, (3) a deflation hollow stabilized by reforestation (forest pl

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30

Lindbo, D. L., and P. L. M. Veneman. "Micromorphology of Selected Massachusetts Fragipan Soils." Soil Science Society of America Journal 57, no. 2 (1993): 437–42. http://dx.doi.org/10.2136/sssaj1993.03615995005700020025x.

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31

曹, 婷婷. "Significance of Soil Micromorphology Research in Land Engineering." Hans Journal of Agricultural Sciences 11, no. 03 (2021): 203–6. http://dx.doi.org/10.12677/hjas.2021.113030.

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32

van Mourik, J. M. "The use of micromorphology in soil pollen analysis." CATENA 35, no. 2-4 (1999): 239–57. http://dx.doi.org/10.1016/s0341-8162(98)00103-9.

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33

RABENHORST, M. C., and K. C. HAERING. "SOIL MICROMORPHOLOGY OF A CHESAPEAKE BAY TIDAL MARSH." Soil Science 147, no. 5 (1989): 339–47. http://dx.doi.org/10.1097/00010694-198905000-00004.

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34

Proebsting, Eric. "The Use of Soil Micromorphology at Sylvester Manor." Northeast Historical Archaeology 36, no. 1 (2007): 71–82. http://dx.doi.org/10.22191/neha/vol36/iss1/7.

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35

Magaldi, D., M. Giammatteo, and P. Smart. "Soil micromorphology of clayey hill slopes, central Italy." Bulletin of Engineering Geology and the Environment 61, no. 4 (2002): 357–62. http://dx.doi.org/10.1007/s10064-002-0158-1.

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36

Carpentier, Frank, and Bruno Vandermeulen. "High-Resolution Photography for Soil Micromorphology Slide Documentation." Geoarchaeology 31, no. 6 (2016): 603–7. http://dx.doi.org/10.1002/gea.21563.

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37

SANTOS, M. C. D., A. R. MERMUT, D. W. ANDERSON, and R. J. ST. ARNAUD. "MICROMORPHOLOGY OF THREE GRAY LUVISOLS IN EAST-CENTRAL SASKATCHEWAN." Canadian Journal of Soil Science 65, no. 4 (1985): 717–26. http://dx.doi.org/10.4141/cjss85-077.

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Micromorphology of three Gray Luvisolic soils under Boreal Forests occurring on late Wisconsinan age glacial till were studied. Profiles 1 and 2 occurred on loam with 8–10% carbonates; Profile 3 on clay loam till with 58% carbonates. The presence of various fecal pellets shows the importance of soil fauna in the decomposition of litter and the formation of aggregates in organic horizons. Aggrotubules and fecal pellets in the lower part of the profiles testified to the presence of biological activity even at depth. Several types of banded fabrics and iron-manganese nodules were observed, and ar

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38

Yakovenko, V. M. "The influence of deluvial processes on macro- and micromorphology of ravined forest soil." Fundamental and Applied Soil Science 15, no. 3-4 (2014): 74–88. http://dx.doi.org/10.15421/041419.

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The paper presents the results of studying the effect of deluvial processes on the formation of macro- and micromorphological properties of forest soils on the example of ravined biogeocenoses of Dnieper Prysamarya. Ravined forest biogeocenoses have a long history of development associated with the evolution of land cover in Postpleistocene epoch. One of the factors of soil formation in ravines is deluvial process as a natural phenomenon typical for the landscapes of the present steppes. Ravined forest soils in the catena in the upper reaches of the ravine Glyboky have been studied. They are s

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39

Singer, A., WFA Kirsten, and C. Buhmann. "Clay dispersivity and crusting of soils determined by Buchner funnel extractions." Soil Research 32, no. 3 (1994): 465. http://dx.doi.org/10.1071/sr9940465.

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Soil dispersivity tests strongly disturb soils and therefore only remotely reproduce conditions in the field. A quick and inexpensive laboratory method for the assessment of clay dispersivity of soils is proposed that involves a much milder soil treatment. The method is based on the observation that, during the separation of the soil solution from soil pastes, the separated soil solution in some soils contains suspended fine matter. The method involves the consecutive extraction of wetted and only mildly disturbed soil packed in a Buchner funnel, under standardized conditions. The time needed

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40

Kok, H., and P. Buurman. "Soil formation on mafic rocks of north Galicia, Spain. 2. Soil micromorphology." Netherlands Journal of Agricultural Science 33, no. 1 (1985): 64–66. http://dx.doi.org/10.18174/njas.v33i1.16875.

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41

Kremin, Nadiya, Andriy Bogucki, and Olena Tomeniuk. "Micromorphology and paleogeographical conditions of formations of the Horokhiv fossil soil complex of the Podolian upland." Visnyk of the Lviv University. Series Geography, no. 50 (December 28, 2016): 224–33. http://dx.doi.org/10.30970/vgg.2016.50.8708.

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The Horokhiv fossil soil complex was formed during the Eemian interglacial and early interstadials of the Upper Pleistocene (MIS 5) within the Podolian Upland. It can be considered as a marking horizon which is quite easy to diagnose. During the Eemian interglacial forest soil was formed and during the early interstadials of the Upper Pleistocene, there were formed three low-thickness and mainly chernozems-like soils which were highly deformed by delluvial-solifluctional processes. These interstadial soils had been called the Kolodiiv soils. All the Kolodiiv soils currently are described only

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42

VandenBygaart, A. J., R. Protz, and A. D. Tomlin. "Changes in pore structure in a no-till chronosequence of silt loam soils, southern Ontario." Canadian Journal of Soil Science 79, no. 1 (1999): 149–60. http://dx.doi.org/10.4141/s98-034.

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Many research studies have dealt with the influences of minimum or no-till soil management practices on the major physical, chemical, biological and morphological properties in the soil profile. However little work has been done on the assessment of the rates of changes in pore properties as management practices are converted from conventional to no-till (NT) methods. Short-term changes in soil micromorphology attributed to conversion to no-till from conventionally tilled management are evaluated in this paper. As the number of years in no-till increased there was a decrease in the number pore

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43

Bush, Richard T., and Leigh A. Sullivan. "Pyrite micromorphology in three Australian Holocene sediments." Soil Research 37, no. 4 (1999): 637. http://dx.doi.org/10.1071/sr98113.

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The distribution and morphology of pyrite in 3 Holocene estuarine sediments were examined using light microscopy, analytical scanning electron microscopy, and X-ray diffraction. The distribution and morphologies of pyrite were similar with pyrite being dispersed throughout the soil matrices as well as concentrated in root remnants and other macropores. The pyrite occurred in both framboidal and irregularly shaped dense clusters from 4 to 15 µm diameter, and also in loose clusters. Individual crystals in these clusters ranged in size from 1 to 2 µm. Pyrite crystals exhibited octahedral, pyritoh

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44

Poch, Rosa M., and Fabio Scarciglia. "Preface: 15th International Conference on Soil Micromorphology (ICSM 2016)." Boletín de la Sociedad Geológica Mexicana 71, no. 1 (2019): i—iii. http://dx.doi.org/10.18268/bsgm2019v71n1p1.

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45

Herrero, J., J. Porta, and N. Fédoroff. "Hypergypsic Soil Micromorphology and Landscape Relationships in Northeastern Spain." Soil Science Society of America Journal 56, no. 4 (1992): 1188–94. http://dx.doi.org/10.2136/sssaj1992.03615995005600040031x.

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46

FITZPATRICK, E. A. "THE USE OF THE TERM BIREFRINGENCE IN SOIL MICROMORPHOLOGY." Soil Science 147, no. 5 (1989): 357–60. http://dx.doi.org/10.1097/00010694-198905000-00006.

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47

Kooistra, Maja J., and Laura I. Kooistra. "Integrated research in archaeology using soil micromorphology and palynology." CATENA 54, no. 3 (2003): 603–17. http://dx.doi.org/10.1016/s0341-8162(03)00137-1.

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48

Mosaferi, Samaneh, та Maryam Keshavarzi. "Epidermal micromorphology of ﬂoret parts in Aeluropus (Poaceae)". Acta Biologica Szegediensis 65, № 1 (2021): 35–45. http://dx.doi.org/10.14232/abs.2021.1.35-45.

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Aeluropus from Poaceae comprises 5 species in the world and 3 species in Iran. This halophytic perennial is distributed in salty and dry soils of Asia, Europe, and Africa. In addition to being used as fodder, it can stabilize the soil by its rhizome or stolon. These features make Aeluropus a valuable plant. In this study, lemma and palea of 10 populations of Aeluropus were studied micromorphologically by scanning electron microscope (SEM) to determine diagnostic features among species studied. Eight characters as micro-prickle, macro-hair, long cell outline, cork and silica cells, papilla, sal

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49

Monger, H. Curtis, and Henry P. Adams. "Micromorphology of Calcite-Silica Deposits, Yucca Mountain, Nevada." Soil Science Society of America Journal 60, no. 2 (1996): 519–30. http://dx.doi.org/10.2136/sssaj1996.03615995006000020026x.

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50

Thompson, T. L., L. R. Hossner, and L. P. Wilding. "Micromorphology of calcium carbonate in bauxite processing waste." Geoderma 48, no. 1-2 (1991): 31–42. http://dx.doi.org/10.1016/0016-7061(91)90004-d.

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