Abstract

Volcanic sands, that contain relatively high content of dark minerals. can be used as a natural fertilizer. Unfortunately, the amount of the nutrients from this material available for the plant growth is very low. To increase the release of the nutrients to the environment. weathering process of the minerals should be accelerated. The objective of this research was to study the capability of urea and ammonium sulphate (ZA) in increasing the release of cations cel', Mi', K', c,i' and Zn2 from the minerals. Urea and ZA used in this study is not only known as source of N fertilizer but also found destroy the floor of storehouse made from concrete.Volcanic sands from Cimangkok and Ciapus were sieved with 100 mesh sieve and were mixed with each urea or ZA with the rate of 10%, 20% and 33%. The mixture was then 3 months incubated in wet conditions. The amount ofCa2 , Mi. K, Cu2 and Zn1 extracted with aquadest was measured at the r ', 2nd and 3rrl month. Due to the higher acidity, adding df the ZA to the sand from Cimangkok and Ciapus effectively increased the amountof extracted C a2 , Mi' and K' compared to the adding of urea. A t the rate of 10%, adding of the ZA to the sand from Ciapusincreased the amount of extracted Ca2 from 25.3 mg kg"! to 800.1 mg kg"! and K from 10.6 mg kg"! to 108.3 mg kg"l. Thehighest concentration of Mi' was found on the treatment of ZA with the rate of 33%. i.e. from 9.8 mg kg"! to 161.7 mg kg"1 insand from Ciapus. Adding of the urea or of the ZA affected the amount of extracted Cu2 and Zn2 , however there was no trendwhich rate effectively have increased the extracted these cations.

Highlights

  • Urea and ZA used in this study is known as source ofN fertilizer and found destroy the floor ofstorehouse made from concrete

  • Volcanic sands from Cimangkok and Ciapus were sieved with 100 mesh sieve and were mixed with each urea or ZA

  • The mixture was 3 months incubated in wet conditions

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Summary

BAHAN DAN METODA

Bahan yang digunakan untuk penelitian ini adalah pasir dari daerah S. Ciapus terdapat pada formasi geologi Qvsl, yaitu terdiri dari lahar, breksi tufaan dan lapili dari G. Sungai Cimangkok berada pada formasi geologi Qgy, yaitu breksi dan lahar dad G. Serpih tufaan, breksi tufaan dan aglomerat tufaan (Sudjatmiko, 1972). Pasir Cimangkok dan pasir Ciapus berukuran lolos saringan 100 mesh dicuci bersih untuk menghilangkan kontaminan. Campuran pasir dengan urealZA diinkubasi pada kondisi lembab. Pengamatan dilakukan pada bulan ke-I, ke-2 dan ke-3 selama masa inkubasi. Pengamatan dilakukan terhadap pH, kadar nitrogen-NH4, kalsium, magnesium, kalium, tembaga dan seng hasil ekstraksi aquadest (1:10) setelah pengocokan selama satu jam. Kation-kation diukur dengan AAS, sedangkan susunan mineral dalam fraksi pasir halus (125210 mesh) dianalisis dengan bantuan mikroskop polarisasi

HASIL DAN PEMBAHASAN
Paslr Clapus
Paslr Clmangkok
DAFTAR PUSTAKA
Full Text
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