1,479
Views
3
CrossRef citations to date
0
Altmetric
Soil genesis, classification and survey

Properties and classification of volcanic ash soils around Lake Kuwanuma on the eastern footslope of Mt. Funagata in Miyagi prefecture, northeastern Japan

, , &
Pages 848-862 | Received 17 Sep 2013, Accepted 01 Aug 2014, Published online: 10 Sep 2014

Figures & data

Figure 1 Locations of the pedons in the present study. Thick lines approximately indicate the boundaries between different soils except for rocky land on steep slope and a bank of the lake Kuwanuma (National Land Agency Citation1994).

Figure 1 Locations of the pedons in the present study. Thick lines approximately indicate the boundaries between different soils except for rocky land on steep slope and a bank of the lake Kuwanuma (National Land Agency Citation1994).

Table 1 Pedon locations and soil names in the local soil map and Classification of Forest Soil in Japan, United Soil Classification System of Japan

Figure 2 Schematic representation of the soil profiles studied. asl, above sea level.

Figure 2 Schematic representation of the soil profiles studied. asl, above sea level.

Table 2 Morphological and physical properties

Table 3 Chemical properties

Table 4 Properties regarding non-crystalline materials

Figure 3 Vertical distributions of pyrophosphate-extractable aluminum (Alp) and iron (Fep).

Figure 3 Vertical distributions of pyrophosphate-extractable aluminum (Alp) and iron (Fep).

Figure 4 X-ray powder diffraction pattern of the 0.2–0.5-mm fraction prepared from the A horizon of pedon 6. Q, F and C denote quartz, feldspar and cristobalite, respectively. Kα denote alpha line from K shell of copper.

Figure 4 X-ray powder diffraction pattern of the 0.2–0.5-mm fraction prepared from the A horizon of pedon 6. Q, F and C denote quartz, feldspar and cristobalite, respectively. Kα denote alpha line from K shell of copper.

Figure 5 X-ray powder diffraction patterns of the clay fraction from the EB horizon of pedon 6 after (a) magnesium (Mg) saturation, (b) Mg saturation and glycerol solvation, (c) K saturation at room temperature, (d) K saturation and heating at 300°C (e) and K saturation and heating at 550°C. Numerals above the diffraction peaks denote d spacings. Kα denote alpha line from K shell of copper.

Figure 5 X-ray powder diffraction patterns of the clay fraction from the EB horizon of pedon 6 after (a) magnesium (Mg) saturation, (b) Mg saturation and glycerol solvation, (c) K saturation at room temperature, (d) K saturation and heating at 300°C (e) and K saturation and heating at 550°C. Numerals above the diffraction peaks denote d spacings. Kα denote alpha line from K shell of copper.

Table 5 Clay mineralogical properties

Table 6 Soil names according to three recent key-out systems

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.