Granitic Rock as a Reliable Multinutrient Fertilizer

Sherif Mansour¹ and Amr Elkelish^2,

¹Geology Department, Faculty of Science, Port Said University, Port Said 42522, Egypt

²Botany Department, Faculty of Science, Suez Canal University, Ismailia 41522, Egypt

Cite this paper

Sherif Mansour and Amr Elkelish. Granitic Rock as a Reliable Multinutrient Fertilizer. World Journal of Agricultural Research. 2021; 9(1):42-46. doi: 10.12691/WJAR-9-1-7

Abstract

Granite is the main component of the continental crust that is exposed over ca. 15 % of the continents. It is composed mainly of aluminosilicate minerals, rich in a variety of elements/nutrients. In Egypt, it outcrops along the Red Sea margin, Southern Sinai, Aswan, and southern the Western Desert. Weathered, fractured, and defective granites are easy to mine and inexpensive. Additionally, the granitic slurry and rock dust which result from cutting and polishing during the granitic manufacturing processes are considered waste products causing a problem and additional industrial costs. Reusing this waste product would benefit the manufacturer. On the other hand, the world's popularity as well as the Egyptian continues to increase at an alarming rate. Consequently, the food demand increases substantially. Egypt has a plan, already in action, for desert reclamation, however, these soils are poor in many fundamental nutrients. Additionally, the natural fertilization of the traditionally planted lands in the Nile Valley and the Delta decreases gradually since the establishment of the High Dam. Moreover, the worldwide high inflation rates cause a huge increase in the chemical fertilizers prices. Therefore, there is an urge and demand for affordable, available, and nutrients rich fertilizers. Granite, is traditionally, used as a potassium fertilizer which could enhance soil quality. However, its nature as an insoluble silicate-based mineral has limited the plants' beneficiary from its fertilizer. During this study, we have designed a strategy by which choosing the most suitable granitic rock type, overcoming its solubility issues, and testing its effect on plants. The treated sample is a monzogranite from the Younger granite suite of the Arabian-Nubian Shield at Somr ElQaa area in the northern Eastern Desert. The monzogranite rocks are generally characterized with minimum silica content among the granitic rocks and roughly equal concentrations of potassium and calcium.

Keywords

granitic fertilizer, mineral fertilizer, soil enrichment, Multinutrient fertilizer

Copyright

This work is licensed under a Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

References

[1]	Twidale, C.R. 2000. Granite outcrops: their utilisation and conservation. Journal of the Royal Society of Western Australia, 83:115-122.
[2]	Stern, R.J., Hedge, C.E., 1985. Geochronologic and isotopic constraints on late Precambrian crustal evolution in the Eastern Desert of Egypt. American Journal of Science 285, 97-127.
[3]	FAO. 2005. Fertilizer use by crop in Egypt. Report of Land and Plant Nutrition Management Service Land and Water Development Division, FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS, Rome, 57pp.
[4]	Tawfik, H.A, Ghandour, I.M, Maejima, W, Abdel-Hameed, A.T. 2011. Petrography and Geochemistry of the Lower Paleozoic Araba Formation, Northern Eastern Desert, Egypt: Implications for Provenance, Tectonic Setting and Weathering Signature. Journal of Geoscience, Osaka City University, 54, 1-16.
[5]	Coroneos, C., Hinsinger, P. Gilkes, R.J. 1995. Granite powder as a source of potassium for plants: a glasshouse bioassay comparing two pasture species. Fertilizer research, 45(2), 143-152.
[6]	Khan, M.A., Rana, H. 2020. Granite Slurry: A Valued By-Product as Fertilizer. International Journal of Research and Innovation in Applied Science (IJRIAS) | Volume V, Issue IV, ISSN 2454-6194.
[7]	Bolland, M. D. A., & Baker, M. J. 2000. Powdered granite is not an effective fertilizer for clover and wheat in sandy soils from Western Australia. Nutrient Cycling in Agroecosystems, 56(1), 59-68.
[8]	MALR. 2003. Bulletin of Agriculture Economics, Central Administration of Agriculture Economics, Ministry of Agriculture and Land Reclamation, published data.
[9]	Kröner, A. 1979. Pan African Plate Tectonics and Its Repercussions on the Crust of Northeast Africa. Geol. Rundsch. 68, 565-583.
[10]	Meert, J.G. 2003. A Synopsis of Events Related to the Assembly of Eastern Gondwana. Tectonophysics, 362, 1-40.
[11]	Engel, A.E.J.; Dixon, T.H.; Stern, R.J. 1980. Late Precambrian Evolution of Afro-Arabian Crust from Ocean Arc to Craton. Geol. Soc. Am. Bull., 91, 699, 2.
[12]	Johnson, P.R.; Andresen, A.; Collins, A.S.; Fowler, A.R.; Fritz, H.; Ghebreab, W.; Kusky, T.; Stern, R.J. 2011. Late Cryogenian–Ediacaran History of the Arabian–Nubian Shield: A Review of Depositional, Plutonic, Structural, and Tectonic Events in the Closing Stages of the Northern East African Orogen. J. Afr. Earth Sci., 61, 167-232.
[13]	Mansour, S. E. E. (2015). Long-term topographic evolution of the African plate, causes and 456 consequences for surrounding lithospheric plates.
[14]	El-Gaby, S.; el-Nady, O.; Khudeir, A. 1984. Tectonic Evolution of the Basement Complex in the Central Eastern Desert of Egypt. Geol. Rundsch., 73, 1019-1036.
[15]	Bentor, Y.K. 1985. The Crustal Evolution of the Arabo-Nubian Massif with Special Reference to the Sinai Peninsula. Precambrian Res., 28, 1-74.
[16]	El Din, G.M.K.; Khudeir, A.A.; Greiling, R.O. 1991. Tectonic Evolution of a Pan-African Gneiss Culmination, Gabal El Sibai Area, Central Eastern Desert, Egypt. Zent Bl Geol Palaeont, I11, 2637-2640.
[17]	Hume, W.F. 1935. The Later Plutonic and Minor Intrusive Rocks, Survey of Egypt, Cairo.
[18]	Schurmann, H.M.E. 1953. The Precambrian of the Gulf of Suez Area. Int Geol Congr Algiers CR, 19, 115-135.
[19]	El Ramly, M.F.; Akaad, M.K. 1960. The Basement Complex in the Central-Eastern Desert of Egypt between Lat. 24°30 and 25° 40 N. Geol. Surv. Egypt Ann., 8.
[20]	Ali, B.H.; Wilde, S.A.; Gabr, M.M.A. 2009. Granitoid Evolution in Sinai, Egypt, Based on Precise SHRIMP U–Pb Zircon Geochronology. Gondwana Research, 15, 38-48.
[21]	Moreno, J.A.; Montero, P.; Abu Anbar, M.; Molina, J.F.; Scarrow, J.H.; Talavera, C.; Cambeses, A.; Bea, F. 2012. SHRIMP U–Pb Zircon Dating of the Katerina Ring Complex: Insights into the Temporal Sequence of Ediacaran Calc-Alkaline to Peralkaline Magmatism in Southern Sinai, Egypt. Gondwana Research, 21, 887-900.
[22]	Said, R. 1990. The Geology of Egypt; 2nd ed.; A.A. Balkema, Rotterdam: Netherlands.
[23]	Seilacher, A. 1990. Paleozoic Trace Fossils. In Geology of Egypt; A.A. Balkema, Rotterdam: Netherlands, pp. 113-156.
[24]	Bosworth, W.; Huchon, P.; McClay, K. 2005. The Red Sea and Gulf of Aden Basins. Journal of African Earth Science. 43, 334-378.
[25]	Stampfii, G.M.; von Raumer, J.F.; Borel, G.D. 2002. Paleozoic Evolution of Pre-Variscan Terranes: From Gondwana to the Variscan Collision. In Variscan-Appalachian dynamics: The building of the late Paleozoic basement; Geological Society of America.
[26]	Craig, J.; Sutcliffe, O.; Lüning, S.; Le Heron, D.; Whittington, R. 2008. Structural Styles and Prospectivity in the Precambrian and Palaeozoic Hydrocarbon Systems of North Africa. In Geology of East Libya; Earth Sci. Soc. of Libya: Tripoli, pp. 51-122.
[27]	Dixon, R.J.; Moore, J.K.S.; Bourne, M.; Dunn, E.; Haig, D.B.; Hossack, J.; Roberts, N.; Parsons, T.; Simmons, C.J. 2010. Integrated Petroleum Systems and Play Fairway Analysis in a Complex Palaeozoic Basin: Ghadames-Illizi Basin, North Africa. Geol. Soc. Lond. Pet. Geol. Conf. Ser., 7, 735-760.
[28]	Said, R. 1962. The Geology of Egypt; 1st ed.; Elsevier, Amsterdam: Netherlands.
[29]	Klitzsch, E. 1986. Plate Tectonics and Cratonal Geology in Northeast Africa (Egypt, Sudan). Geol. Rundsch., 75, 755-768.
[30]	Hashad, A.H. 1978. Present Status of Geochronological Data on the Egyptian Basement Complex. Precambrian Research, 6, A24-A25.
[31]	Greiling, R.O.; Kriiner, A.; El Ramly, M.F.; Rashwan, A.A. 1988. Structural Relationships between the Southern and Central Parts of the Eastern Desert of Egypt: Details of a Fold and Thrust Belt. In The Pan-African of NE Africa and Adjacent Areas; El Gaby, S., Greiling, R.O., Eds.; Vieweg: Wiesbaden, pp. 121-145.
[32]	Hassan, M.A.; Hashad, A.H. 1990. Precambrian of Egypt. In Geology of Egypt; Said, R., Ed.; Balkema Publications, Netherlands, p. 734.