PEDO-TRANSFER FUNCTIONS AND MAPPING OF FE IN WHEAT SEED UNDER SOUTH PARTS FARMS OF KHOUZESTAN

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

GHOLAMI A.; JAFARNEJADI A.R.; SAYYAD GH.; DAVAMI A.H.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: CROP PHYSIOLOGY Year:2010 | Volume:2 | Issue:3 Page(s): 45-57

Download Full-Text

Persian Verion

View:

877

Download:

Cites:

Information Journal Paper

Title

PEDO-TRANSFER FUNCTIONS AND MAPPING OF FE IN WHEAT SEED UNDER SOUTH PARTS FARMS OF KHOUZESTAN

Author(s)

GHOLAMI A. | JAFARNEJADI A.R. | SAYYAD GH. | DAVAMI A.H. | Issue Writer Certificate

Keywords

IRONQ2

MAPPINGQ2

PEDO-TRANFER FUNCTIONQ3

WHEATQ3

Abstract

This research was conducted for preparing pedo - transfer functions and MAPPING of -IRON (Fe) on seed and WHEAT farms soils of some regions Khuzestan province. In order to, at maturity growth stage of WHEAT, 121 samples (soil and WHEAT) were taken from Ahvaz, Dasht-e-Azadegan, Hendijan, Khoramshar, Mahshar, Shadegan, Ramhormoz and Omedeyeh using a weighing method. All samples (seed and soil) were analyzed for soil properties and Fe of seed. The results revealed that Fe concentrations average on seed and soil were measured 56.5 and 12.56 (mg.kg-1) respectively. Also, more than 50% soils, Fe-DTPA concentration was less than 10 (mg.kg-1). A significant correlation was obtained between the seed-Fe and soil salinity (r=0.74*). There was significant (p<0.05) correlation between DTPA-Fe and Clay content (r=0.73*), cation exchange capacity (CEC) (r=0.82*), P-available (r=0.82*) and EC (p<0.01) (r=0.86**) of the soils. Hence, The soil salinity had main role on soil- Fe bioavailability for plant uptake. The regression pedo-trasfer function showed that seed Fe concentration depended on sol salinity, P-available and CEC (R2=0.96). The semivariograms of seed and soil Fe concentrations revealed spherical model can explain seed and soil Fe spatial variability in study regions.

Cites

No record.

References

Cite

APA: Copy

GHOLAMI, A., JAFARNEJADI, A.R., SAYYAD, GH., & DAVAMI, A.H.. (2010). PEDO-TRANSFER FUNCTIONS AND MAPPING OF FE IN WHEAT SEED UNDER SOUTH PARTS FARMS OF KHOUZESTAN. CROP PHYSIOLOGY, 2(3), 45-57. SID. https://sid.ir/paper/174475/en

Vancouver: Copy

GHOLAMI A., JAFARNEJADI A.R., SAYYAD GH., DAVAMI A.H.. PEDO-TRANSFER FUNCTIONS AND MAPPING OF FE IN WHEAT SEED UNDER SOUTH PARTS FARMS OF KHOUZESTAN. CROP PHYSIOLOGY[Internet]. 2010;2(3):45-57. Available from: https://sid.ir/paper/174475/en

IEEE: Copy

A. GHOLAMI, A.R. JAFARNEJADI, GH. SAYYAD, and A.H. DAVAMI, “PEDO-TRANSFER FUNCTIONS AND MAPPING OF FE IN WHEAT SEED UNDER SOUTH PARTS FARMS OF KHOUZESTAN,” CROP PHYSIOLOGY, vol. 2, no. 3, pp. 45–57, 2010, [Online]. Available: https://sid.ir/paper/174475/en

Related Journal Papers