Detailed soil survey of the north-eastern portion of ASRCT Sakaerat Experiment Station (Amphoe Pak Thong Chai, Changwat Nakhon Ratchasima) / F. Bos, Vichit Thunduan
โดย: Bos. F.
ผู้แต่งร่วม: Thunduan, Vichit | Thailand Institute of Scientific and Technological Research
Language: English ชื่อชุด: Res. Proj. no. 27/1 ; Rep. no. 1ข้อมูลการพิมพ์: Bangkok : Thailand Institute of Scientific and Technological Research, 1968 รายละเอียดตัวเล่ม: 22 p.หัวเรื่อง: Nakhon Ratchasima | Sakaerat Environmental Research Station | Soil surveys | Soilsสารสนเทศออนไลน์: Click here to access full-text สาระสังเขป: A detailed survey of the soils of an area of about 12 km in the north-east portion of the ASRCT Sakaerat Experiment Station has been undertaken to provide soils data for an interdisciplinary study of a dry-evergreen tropical forest environment. The majority of the soils belong to the Red-Yellow Podzolic great soil group, occurring in all topographic positions on materials derived from both sandstone and shale. Soil series included are Khao Yai series, covering the deep soils, occurring in the dry-evergreen forest; Muak Lek series, covering the deeper soils on shale-derived material, differing from the Khao Yai series in the yellow colour and the presence of mottles; Tha Yang series, covering all soils with a stoniness of 1 or higher. Some of the soils may belong to the Reddish Brown Lateritic great soil group, but their occurrence is incidental, and the soils observed appear to the transitional to the Red-Yellow Podzolic soils. Low-Humic Gley soils are found in a few poorly drained depressions and are formed on colluvium and residum of sandstone and shale. Soil conditions in the survey area are estimated to be fairly representative of general soil conditions in the hilly parts of south-east Asia, and of Thailand in particular S.K
| ชนิดของทรัพยากร | Location | Call number | สถานะ | Last seen | Copy No. | บาร์โค้ด |
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วว. เทคโนธานี | Checked out | 2018-11-08 | 1 | RP1968/202 | |
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วว. เทคโนธานี | Available | 2018-08-31 | 2 | RP1968/202-2 |
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