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Image of KERAGAMAN NILAI KETERHANTARAN HIDROLIK TANAH PADA LAHAN RAWA PASANG SURUT PETAK TERSIER 8 (TC 8) P8-2S, DESA TELANG JAYA, KECAMATAN MUARA TELANG, KABUPATEN BANYUASIN

Text

KERAGAMAN NILAI KETERHANTARAN HIDROLIK TANAH PADA LAHAN RAWA PASANG SURUT PETAK TERSIER 8 (TC 8) P8-2S, DESA TELANG JAYA, KECAMATAN MUARA TELANG, KABUPATEN BANYUASIN

Arganta, Donni - Personal Name;

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Soil hydraulic conductivity is the ability of the soil to drain or pass water in a layer or soil profile in a certain time interval. This study aims to study the value of the diversity of soil hydraulic conductivity and how the influence of soil physical properties on soil hydraulic conductivity on tidal land. This research was carried out in plots 4 and 8 tertiary 8 P8-2S, Telang Jaya Village, Muara Telang District, Banyuasin Regency. The method used in this research is a survey method with direct field observation then analysis is carried out in the laboratory. The research area is 16 Ha. Measurement of the hydraulic conductivity of saturated soil in the field using the Auger Hole Method. Each observation area is taken 8 sample points so that there are 16 observation sample points and the depth of each auger hole is 60 cm. Measurement of the rate of rise of the ground water level was repeated 3 times. The results of measuring the value of K-hydraulic in the field using the Auger Hole Method. For the highest value is in plot 4, sample point 7 is 16.29 cm/hour-1 with the K-hydraulic class fast criteria, for the low K-hydraulic value is located in plot 4 sample point 2 is 2.45 cm/hour-1 with medium K-hydraulic class criteria. The results of the standard deviation of K values from the two research variables obtained, namely plots 4 and plots 8 have different K standard deviation values where in plot 4 the K value standard deviation is 4.91 cm/hour-1 and in plot 8 the K value standard deviation is 1.8 cm/hour-1. Soil physical properties that have a positive effect on the rate of soil hydraulic conductivity are soil texture and soil pore space, on the other hand, soil density has a negative effect on hydraulic K.


Availability
Inventory Code Barcode Call Number Location Status
2107004118T58915T589152021Central Library (Referens)Available but not for loan - Not for Loan
Detail Information
Series Title
-
Call Number
T589152021
Publisher
Inderalaya : Prodi Ilmu Tanah, Fakultas Pertanian Universitas Sriwijaya., 2021
Collation
viii, 39 hlm. : ilus. ; 29 cm
Language
Indonesia
ISBN/ISSN
-
Classification
631.407
Content Type
-
Media Type
-
Carrier Type
-
Edition
-
Subject(s)
Konservasi Tanah
Prodi Ilmu Tanah
Specific Detail Info
-
Statement of Responsibility
SEPTA
Other version/related

No other version available

File Attachment
  • KERAGAMAN NILAI KETERHANTARAN HIDROLIK TANAH PADA LAHAN RAWA PASANG SURUT PETAK TERSIER 8 (TC 8) P8-2S, DESA TELANG JAYA, KECAMATAN MUARA TELANG, KABUPATEN BANYUASIN
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