GENESIS AND MORPHOLOGY OF ARGILLIC HORIZONS IN SOME SEMIARID SOILS IN THE WEST OF URMIA LAKE

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

MANAFI SH.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: Journal of Soil Management and Sustainable Production Year:2015 | Volume:5 | Issue:3 Page(s): 145-160

Download Full-Text

Persian Verion

View:

1,543

Download:

Cites:

Information Journal Paper

Title

GENESIS AND MORPHOLOGY OF ARGILLIC HORIZONS IN SOME SEMIARID SOILS IN THE WEST OF URMIA LAKE

Author(s)

MANAFI SH. | Issue Writer Certificate

Keywords

ARGILLIC HORIZONQ2

CLAY SKINQ2

CLIMATE CHANGEQ2

MICROMORPHOLOGYQ1

POLYGENESISQ2

Abstract

Background and Objectives: ARGILLIC HORIZONs are subsurface horizons which contain considerably more phylosilicate clays than upper horizons show evidences of clay illuviation.In some soils evidences of illuviation of clay are obvious, whereas, some soils due to weathering and insitu formation of clay particles, evidences of clay illuviation disappear. Under such circumstances, as a key tool, MICROMORPHOLOGY properly helps for recognition of ARGILLIC HORIZONs.Materials and Methods: In this study ARGILLIC HORIZONs in calcareous soils of a semiarid region, with xeric and mesic soil moisture and temperature regimes, in the west of Urmia Lake were studied. Thus, a toposequence in different physiographic positions including piedmont plains, plateau, hills and mountains was investigated. In each land type, three soil profiles were dug and described and their morphological properties were determined. Disturbed samples for physical and chemical studies and undisturbed and oriented samples for micromorphological studies were obtained from characteristic horizons. Physical and chemical properties of soils were determined using standard methods. In order to perform micromorphic studies, thin sections with the thickness of 25-30 microns were prepared from undisturbed and oriented samples and were studied using polarizing microscope under cross polarized (XPL) and plain polarized (PPL) lights.Results: Field observations revealed the presence of ARGILLIC HORIZONs only in piedmont plains and plateau land types and the physico-chemical and micromorphological results confirmed their presence as well. According to the results, ARGILLIC HORIZONs had redder Hue, higher clay content and ratio of fine clay to total clay than the overlying horizons. Thin section observations showed that CLAY SKINs are present as coatings with a thickness of 0.08-0.34 mm on the faces of voids and skeletal grains and comprise 2-7% of thin sections of ARGILLIC HORIZONs and in some cases, they have filled all of pore spaces. Regarding to semiarid climate of this region and presence of high quantities of calcium carbonate equivalent in these soils, the genesis of ARGILLIC HORIZONs in this region was probably related to the wetter past climate and thus, ARGILLIC HORIZONs in these soils are relict features from a wetter climate in lower Quaternary. In some of these studied soils clay coatings have been engulfed by calcium carbonate and in some cases, they have been disappeared completely. The engulfment of clay coatings by calcium carbonate shows that the climate of this region has been changed from wet to arid which caused to calcium carbonate accumulation in ARGILLIC HORIZONs and changing them to the complex argillic- calcic horizons and thus, these soils are polygenetic.Conclusion: Presence of ARGILLIC HORIZONs in these soils shows that this region was geomorphologically stable and the stability of this area along with other suitable condition for translocation of clay particles in profile (such as wetter climate) have led to formation ARGILLIC HORIZONs in this area.

Cites

No record.

References

No record.

Cite

APA: Copy

MANAFI, SH.. (2015). GENESIS AND MORPHOLOGY OF ARGILLIC HORIZONS IN SOME SEMIARID SOILS IN THE WEST OF URMIA LAKE. ELECTRONIC JOURNAL OF SOIL MANAGEMENT AND SUSTAINABLE PRODUCTION, 5(3), 145-160. SID. https://sid.ir/paper/209801/en

Vancouver: Copy

MANAFI SH.. GENESIS AND MORPHOLOGY OF ARGILLIC HORIZONS IN SOME SEMIARID SOILS IN THE WEST OF URMIA LAKE. ELECTRONIC JOURNAL OF SOIL MANAGEMENT AND SUSTAINABLE PRODUCTION[Internet]. 2015;5(3):145-160. Available from: https://sid.ir/paper/209801/en

IEEE: Copy

SH. MANAFI, “GENESIS AND MORPHOLOGY OF ARGILLIC HORIZONS IN SOME SEMIARID SOILS IN THE WEST OF URMIA LAKE,” ELECTRONIC JOURNAL OF SOIL MANAGEMENT AND SUSTAINABLE PRODUCTION, vol. 5, no. 3, pp. 145–160, 2015, [Online]. Available: https://sid.ir/paper/209801/en

Related Journal Papers