𝔖 Bobbio Scriptorium
✦   LIBER   ✦

A developed DNA extraction method for different soil samples

✍ Scribed by Yingchang Hu; Zhiheng Liu; Jianfang Yan; Xiaohui Qi; Jing Li; Shiqi Zhong; Jicheng Yu; Qiu Liu


Publisher
John Wiley and Sons
Year
2010
Tongue
English
Weight
418 KB
Volume
50
Category
Article
ISSN
0233-111X

No coin nor oath required. For personal study only.

✦ Synopsis


Abstract

Four DNA extraction methods namely SDS‐hyperhaline method (I), modified SDS‐hyperhaline method (II), indirect method (III), alkaline lysis method (IV) were evaluated by comparing DNA yield, spectrophotometric quality, genomic integrity and PCR suitability in this paper. The results showed that high DNA yields were obtained by method I, II and IV. However, higher quality of DNA was gained by method III and IV. Based on the results of the Pulsed‐Field Gel Electrophoresis (PFGE), the completeness of DNA extracted by method IV was the best. About 6.0 μg DNA can be recovered from 1.0 g soil by method IV which involved to lysis cell by SDS and to precipitate impurities by adding potassium acetate and magnesium chloride Therefore, it is confirmed that method IV is a novel, reliable and versatile method for large‐scale DNA extraction involving less purification steps for various soil samples. (© 2010 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)


📜 SIMILAR VOLUMES


Improved method for morphine extraction
✍ G. L. Sprague; A. E. Takemori 📂 Article 📅 1979 🏛 John Wiley and Sons 🌐 English ⚖ 371 KB

0 Methadone, morphine, or naloxone extraction from brain homogenates, plasma, and urine is described. An aqueous sample was loaded on a surgical gauze support, which was washed with extracting solvents. Aqueous samples remained on the support, and nonpolar drugs partitioned into the lipophilic extra

A finite difference method for measuring
✍ J. D. Coleman 📂 Article 📅 1984 🏛 John Wiley and Sons 🌐 English ⚖ 298 KB

A method is devised for measuring soil thermal diffusivity in situ. It is based on direct experimental simulation of the finite difference approximation to the one-dimensional heat conduction equation. The method does not require the soil to be homogeneous except between the three thermometers that