RANCHLAND FORMED in production
Zone named LA PATRIA /INFANTE RIVAROLA
BOQUERON - CHACO –
PARAGUAY
Quantity of
hectares: 10,000. (24.000 acres)
Quantity of
Acres of Pasture Gatton Panic: 4,500.(10.800 acres)
Pasture
State: Very Good paddocks and other good, 30% of total weeds, cleaning
equipment working on their total recovery.
Water
Quality: Excellent.
Soil Type:
Ideal for Livestock.
37 paddocks.
More than 160
km of wiring, Perimeter and Internal 5-wire 4-wire, all posts quebracho (Schinopsis balansae) and palo
santo ( Bulnesia
Sarmientoi)
Kilometers of
Internal Roads: 60.
Internal
Roads Status: Very Good.
Withdrawals:
1.
Corrals: 1,
to 2,000 cattle. (with Pier, pool bath, Storage, Roofing, Illuminated, etc..).
Complete
systems for small animals (goats, sheep, porcine, poultry).
4 Large NATURAL
WATER RESERVOIR 60,000 m3, 50,000 m3, 50,000 m3, 30,000 m3, respectively, all
with Australian tank 150 m3 and Windmill.
1 Large NATURAL
WATER RESERVOIR 20,000 m3 (Australian Tankless).
12 NATURAL
WATER RESERVOIR less than 20,000 m3.
7 Artesian
Wells Drilled, drilled to about 220 feet deep. 3 of them have reinforced
concrete structure, Glass Fiber Tank 15,000 liter diesel engine compressor, one
of them has a separate mains three-phase medium voltage (1,000 meters), and 25
KVA transformer.
Workshop barn,
Sawmill, Deposits, other: 1.400 m2. Complete equipment Sawmill.
Employers
House in excellent condition, with 4 bedrooms, 1 master suite with dressing
room and bathroom, 1 en suite, 2 with shared bathroom, garage for a big truck,
barbecue grill, 1 dining room, a large living room with a fireplace, wide
corridors, etc..
3 large
personal homes, plus 1 retirement.
1 landing strip 1,200 meters long and 60 meters
wide, registered in the National Civil Aviation – Dirección Nacional de
Aeronáutica Civil (DINAC).
Environmental
Impact Study approved SEAM day.
Obs:
The property is located on asphalted road ( Bioceanico Corridor, which connects
Brazil to Chile) 678 km from Asuncion, with 10 kilometers of front about the
same, 35 Kms from the Estancia La Patria, has Electric Energy of ANDE, with
free Medium Voltage, Three Phase Transformer 63 Kva., there is a greater amount
of infrastructure available to the field that is not detailed in this
relatorio, such as: internal Lighting, Underground Pipes for Distribution water
drinkers Ho Ao, etc.. Observation
Highlights: The property is located on a sub-basin Yrenda Aquifer, which
has the best water quality Aquifer giving you plenty of sweet and Drinking
Water.
This ranchland is ready to operate
The most important is located on the aquifer Yrenda
YRENDA ACUIFER
The SAY is a regional hydrogeological system that occupies Paraguay, Argentina, and Bolivia. It is a semi confined to confined aquifer and consists of unconsolidated quaternary and tertiary sediments , that covers ca. 2/3 of the Western Region in Paraguay.
The groundwater salinity increases along the flow direction, which is from W to E; the velocity is estimated in the range of 20 to 46 m/yr. Recharge takes place in the Bolivian region through direct infiltration of precipitation and river water, in the sub-Andean hills (serranía del Aguaragüe). Discharge occurs twofold, depending on the area where it takes place. A) In the central-east region, discharge gives place to wetlands of brackish-salty waters, due to the presence of an impervious barrier to the east that partly avoids the further flow to the Paraguay River. The barrier causes an increase of the rest water level, which lies very close to the surface in the eastern part of the Central Chaco. This situation is not reverted by groundwater extraction for domestic water supply of urban areas because, due to the salinity, extraction is limited. B)The over exploitation of the eastern aquifers allows the intrusion of salty groundwater from the Yrenda Aquifer System into the Eastern Region of Paraguay. The aquifer at the border to Bolivia is characterized by a permeability that varies between 6-8 m/d and a transmissivity in the range of 400-200 m2/d. In the Central Chaco, the permeability lies between 0.3 and 12 m/d and the transmissivity between 80 and 120 m2/d, while the specific capacity varies in the range of 1.1 to 3.7 m3/h/m. These variations are related to the distribution of the permeable sediments, as grain sizes decrease from west to east following the deposition track.