Previous Page  14 / 36 Next Page
Information
Show Menu
Previous Page 14 / 36 Next Page
Page Background

Page 145

Notes:

conferenceseries

.com

Volume 6, Issue 4 (Suppl)

J Material Sci Eng, an open access journal

ISSN: 2169-0022

Materials Congress 2017

June 12-14, 2017

June 12-14, 2017 Rome, Italy

Materials Science and Engineering

9

th

World Congress on

Preparation of zeolite for slow-release fertilizer using K-feldspar powder

Jiangyan Yuan

China University of Geosciences, China

T

he 30-50% of crop yields is attributed to the commercial chemical fertilizers according to conservative estimation. Abuse of

chemical fertilizers causes serious contamination and environmental hazards, and very low amount of nutrition is absorbed by

the plants. The utilization of slow release fertilizer can slow down the migration rate of nutritional elements, which is beneficial to the

improvement of fertilizer use efficiency and production, as well as the decrease of soil contamination. The global demand of potash has

exceeded 32 million metric tons of K

2

O in current time and will have a continuous increase in the coming decade potassium-bearing

framework aluminosilicate minerals have been proposed as a substitute source of potassium. As a kind of K-zeolite, zeolite F still

provide K element necessary to the growth of plants and amend soil besides the function of retaining water and nutrition. Synthesis

of F zeolites from K-feldspar is one of the promising applications of K elements in soil. The X-ray diffraction (XRD) patterns of zeolite

F(KALSiO4.1.5 H

2

O) obtained by the hydrothermal method after the fusing of K-feldspar. All of the diffraction peaks can be basically

indexed to the tetragonal phases of zeolite F (JCPDS file 38-0216) as shown in Figure 1a. The strongest peak of zeolite F at 30.17º

is assigned to its (114) crystal plane. We can see the morphology of zeolite F from Figure 1b that presents tetragonal cross-shaped

composed of rectangular sheet. According to the test of water solubility, accumulative release of K

2

O can be fitted by the equation

as follows: y=0.6349-0.0157ln(x-0.994), where y is accumulative release of K

2

O (%) and x is test time (days); and the correlation

coefficient R

2

=0.991. which indicates the release of zeolite F belongs to Elovich equation. By the observation and prediction of Figure

1a, the accumulative release of K

2

O reaches 68.97% after water solubility testing for 42 days, 72.09% for 240 days, and 72.75% for 365

days, respectively, indicating the sample could be used as a long-term slow-release potassium fertilizer with nutrient K

2

O release.

Biography

Jiangyan Yuan has her expertise in Material Science and Engineering. Her research interests consist of comprehensive utilization and green processing of

mineral resources, such as hydrothermal leaching of valuable elements, hydrothermal synthesis of zeolite; crystal structure transformation; and preparation and

characterization of nano-materials as well as their application.

yuanjy0609@163.com

Jiangyan Yuan, J Material Sci Eng 2017, 6:4(Suppl)

DOI: 10.4172/2169-0022-C1-068