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Effect of sources and rates of organic matter on the soil aggregate stability and bulk density in the northern Khuzestan

Document Type : Research Paper

Authors

  • Kamran Mirzashahi 1
  • Hasan Rouhipour 2

1 Research Instructor, Khuzestan Agricultural and Natural Resources Research and Education Center, AREEO, Dezfool, Iran

2 Assistant Professor, Desert Research Division, Research Institute of Forests and Rangelands, Agricultural Research, Education and Extension Organization (AREEO), Tehran, Iran

https://doi.org/10.22092/ijrdr.2019.119559

Keywords

  • Organic matter
  • aggregate stability
  • MWD
  • bulk density
Iranian Journal of Range and Desert Research
Volume 12, Issue 4
August 2019
Pages 395-407
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APA

Mirzashahi, K. and Rouhipour, H. (2006). Effect of sources and rates of organic matter on the soil aggregate stability and bulk density in the northern Khuzestan. Iranian Journal of Range and Desert Research, 12(4), 395-407. doi: 10.22092/ijrdr.2019.119559

MLA

Mirzashahi, K. , and Rouhipour, H. . "Effect of sources and rates of organic matter on the soil aggregate stability and bulk density in the northern Khuzestan", Iranian Journal of Range and Desert Research, 12, 4, 2006, 395-407. doi: 10.22092/ijrdr.2019.119559

HARVARD

Mirzashahi, K., Rouhipour, H. (2006). 'Effect of sources and rates of organic matter on the soil aggregate stability and bulk density in the northern Khuzestan', Iranian Journal of Range and Desert Research, 12(4), pp. 395-407. doi: 10.22092/ijrdr.2019.119559

CHICAGO

K. Mirzashahi and H. Rouhipour, "Effect of sources and rates of organic matter on the soil aggregate stability and bulk density in the northern Khuzestan," Iranian Journal of Range and Desert Research, 12 4 (2006): 395-407, doi: 10.22092/ijrdr.2019.119559

VANCOUVER

Mirzashahi, K., Rouhipour, H. Effect of sources and rates of organic matter on the soil aggregate stability and bulk density in the northern Khuzestan. Iranian Journal of Range and Desert Research, 2006; 12(4): 395-407. doi: 10.22092/ijrdr.2019.119559

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