Jumat, 10 April 2015
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Minggu, 05 April 2015
Jumat, 03 April 2015
KEUNGGULAN AZOMITE
- Merupakan produk pupuk asal USA dengan kandungan hara yang sangat lengkap (67 mineral) meliputi hara makro mikro dan trace mineral yang sangat diperlukan untuk pertumbuhan tanaman dan kualitas hasil.
- Sudah terbukti di negara-negara lainnya di ASIA, EROPA, USA dalam mendukung keberhasilan peningkatan produksi pertaniannya
- Mengandung REE (Rare Earth Element) yang memiliki fungsi yang unik dan hanya terdapat di dalam pupuk Azomite
- Memiliki
struktur koloid sehingga menjamin ketersediaan haranya untuk tanaman dan meningkatkan remineralisasi hara di dalam tanah
- Meningkatkan fiksasi Nitrogen dari
udara oleh aktivitas Azotobacter di dalam tanah
- Mengurangi kehilangan hara yang
disebabkan oleh proses leaching, fiksasi tanah dan hara dari dalam tanah
- Meningkatkan efisiensi penyerapan
hara makro dan ketersediaan hara
mikro yang sesuai dengan kebutuhan tanaman
- Meningkatkan daya germinasi
(perkecambahan) dan vigor benih
- Meningkatkan inisiasi perakaran dan
pertumbuhan bibit
- Meningkatkan kadar klorofil dan laju
fotosintesa daun
- Meningkatkan status air dalam
jaringan tanaman sehingga tanaman tidak mudah stress dalam kondisi kekeringan
- Meningkatkan ketahanan tanaman
terhadap hama dan penyakit
- Meningkatkan kualitas daya simpan
hasil panen (umbi dan buah)
- Meningkatkan kestabilan pH tanah
- Mudah dalam aplikasinya, dapat
digunakan sebagai campuran media tanam benih atau bibit, sebagai pupuk dasar, dikocorkan, atau untuk aplikasi
penyemprotan ke daun tanaman
- Dapat dicampurkan dengan pupuk atau
pestisida dalam aplikasinya
- Dapat digunakan sebagai enrichment
(pengkaya unsur hara) untuk pupuk lainnya sehingga menghasilkan produk dengan hara terlengkap dan tepat untuk
kebutuhan tanaman
-Merupakan green product/produk alami
sehingga aman untuk tanaman, ikan, hewan ternak, dan tidak meracuni lingkungan serta sangat sesuai untuk
usaha budidaya pertanian organik
(Azomite - -mendapatkan
sertifikasi organik dari Lembaga Sertifikasi Organik International,
OMRI International-USA)
Kamis, 02 April 2015
AZOMITE VS ZEOLITE
AZOMITE® & Zeolites
AZOMITE® is sometimes mistakenly compared to another type of rock deposit
known as a zeolite. As we shall see, the usage, physical structure and chemical
composition of AZOMITE® is quite distinct from all
zeolites.
There are roughly 40 natural
zeolites in existence today as well as over 100 manmade ones. Natural zeolites
are most commonly used in pet litter to retain waste; in animal feed as a toxin
binder (even though most toxin binding only works well in vitro and
rarely very well in the gut of the animal); in agricultural applications for
soils that have poor water retention qualities; and in wastewater
treatment. In contrast, manmade zeolites are more frequently used for
water treatment as ion-exchange resins or in petroleum cracking to resolve
impurities.
In marked contrast, AZOMITE®’s physical structure, usage profile, and number
of biologically available trace minerals are vastly different from any
zeolite. For example, zeolites have a crystalline structure that provides
very good water retention, while AZOMITE®’s
colloidal structure contributes very little to water retention and appears to
more closely resemble a teardrop in which the trace minerals line the
perimeter. Second, AZOMITE® is used in animal feed
and for soil remineralization where it provides an abundance of trace minerals
that are lacking in many feed ingredients and also missing from agricultural
lands. Many scientific studies using AZOMITE® in
soil and in animal feed suggest that its trace minerals are biologically
available; use of zeolites, on the other hand, only provides chemical
absorption, adsorption or water retention.
There are so many natural
zeolites in existence that it is virtually impossible to provide a reliable
single comparative analysis between all zeolites vs. AZOMITE®, but below is a comparison of some of the trace
minerals in AZOMITE® vs. one example of a natural
zeolite currently on the market. Note that AZOMITE®
is higher in trace elements in every essential mineral except Copper (Cu) and
includes many others that zeolites usually do not possess:
Trace Element
|
AZOMITE®
|
Amount in Common
Zeolite
|
Boron (B)
|
29 ppm
|
0
|
Chromium (Cr)
|
6.1 ppm
|
0
|
Cobalt (Co)
|
22.3 ppm
|
0
|
Iodine (I)
|
2.2 ppm
|
0
|
Molybdenum
(Mo)
|
12.6 ppm
|
0
|
Nickel (Ni)
|
2.6 ppm
|
0
|
Praseodymium
(Pr)
|
27 ppm
|
0
|
Selenium (Se)
|
0.7 ppm
|
0
|
Silver (Ag)
|
0.005 ppm
|
0
|
Sulphur (S)
|
240 ppm
|
0
|
Tin (Sn)
|
2.9 ppm
|
0
|
Vanadium (V)
|
7.8 ppm
|
0
|
Potassium
|
5.23%
|
4.19%
|
Calcium
|
3.67%
|
2.23%
|
Sodium
|
2.07%
|
0.59%
|
Silica
|
65.85%
|
67.40%
|
Aluminia
|
11.43%
|
10.60%
|
Magnesium
|
0.78%
|
0.45%
|
Titania
|
0.20%
|
0.27%
|
Phosphorous
|
0.15%
|
0.10%
|
Manganese
|
0.02%
|
0.01%
|
Copper (Cu)
|
12 ppm
|
25 ppm
|
Zinc (Zn)
|
64.3 ppm
|
35 ppm
|
Rubidium (Rb)
|
325 ppm
|
120 ppm
|
Iron (Fe)
|
1.37%
|
1.30%
|
Zirconium (Zr)
|
62.7 ppm
|
480 ppm
|
Yttrium (Y)
|
23 ppm
|
55 ppm
|
Niobium (Nb)
|
40 ppm
|
40 ppm
|
Strontium (Sr)
|
380 ppm
|
560 ppm
|
Neodymium (Nd)
|
5.1 ppm
|
45 ppm
|
Lanthanum (La)
|
220 ppm
|
55 ppm
|
Barium (Ba)
|
0.09%
|
1200 ppm
|
Cerium (Ce)
|
230 ppm
|
130 ppm
|
Lead (Pb)
|
6.2 ppm
|
29 ppm
|
For more information on
zeolites, see the website maintained by the United States Geological Survey (USGS) here.
 |
AZOMITE® is a unique volcanic deposit with over 67 trace elements. Below are
a few comparisons of different volcanic ash deposits around the world. You can
clearly see that AZOMITE® has a higher concentration
and broader range of trace mineral elements.
Essential Trace Elements
in AZOMITE® vs Two Volcanic Bentonites in Uruguay*
Trace Element
|
AZOMITE®
|
Bentonites
|
Copper (Cu)
|
13.5 ppm
|
4.3 ppm
|
Molybdenum (Mo)
|
12.6 ppm
|
0.05 ppm
|
Chromium (Cr)
|
7.8 ppm
|
1.28 ppm
|
Cobalt (Co)
|
22.3 ppm
|
4.3 ppm
|
Boron (B)
|
29 ppm
|
0 ppm
|
Iodine (I)
|
3.2 ppm
|
0 ppm
|
Selenium (Se)
|
0.79 ppm
|
0 ppm
|
Lanthanum (La)
|
257 ppm
|
47.2 ppm
|
Cerium (Ce)
|
360 ppm
|
94.4 ppm
|
Praseodymium (Pr)
|
27 ppm
|
13.1 ppm
|
Nickel (Ni)
|
2.6 ppm
|
0 ppm
|
Rubidium (Rb)
|
325 ppm
|
6.2 ppm
|
Tungsten
|
31 ppm
|
0.69 ppm
|
Sulphur
|
210 ppm
|
0 ppm
|
*Annals of the Brazilian Academy
of Sciences;
2006 78(3) 525-541; “Chemical Signature of Two
Permian Volcanic Ash Deposits within a bentonite bed from Melo, Uruguay”
2006 78(3) 525-541; “Chemical Signature of Two
Permian Volcanic Ash Deposits within a bentonite bed from Melo, Uruguay”
Properties of Five
Volcanic Ash Deposits from Four Countries** vs. AZOMITE®
Mineral Element
|
AZOMITE®
|
Volcanic Ash
|
Boron (B)
|
29 ppm
|
0.25 ppm
|
Cobalt (Co)
|
22.3 ppm
|
0.03 ppm
|
Copper (Cu)
|
13.5 ppm
|
0.66 ppm
|
Iron (Fe)
|
10,370 ppm
|
2.51 ppm
|
Manganese (Mn)
|
200 ppm
|
5.93 ppm
|
Vanadium (V)
|
9.3 ppm
|
0.09 ppm
|
Zinc (Zn)
|
64.3
|
1.96 ppm
|
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