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UT researchers use simple scaling theory to better predict gas production in barnett shale wells


AUSTIN, Texas — Researchers at The University of Texas at Austin have developed a simple scaling theory to estimate gas production from hydraulically fractured wells in the Barnett Shale. The method is intended to help the energy industry accurately identify low- and high-producing horizontal wells, as well as accurately predict how long it will take for gas reserves to deplete in the wells.

Using historical data from horizontal wells in the Barnett Shale formation in North Texas, Tad Patzek, professor and chair in the Department of Petroleum and Geosystems Engineering in the Cockrell School of Engineering; Michael Marder, professor of physics in the College of Natural Sciences; and Frank Male, a graduate student in physics, used a simple physics theory to model the rate at which production from the wells declines over time, known as the "decline curve."

They describe their new model of the decline curve in the paper "Gas production in the Barnett Shale obeys a simple scaling theory," published this week in the Proceedings of the National Academy of Sciences. To test their theory, the researchers analyzed 10 years of gas production data from the Barnett Shale licensed to the university by IHS CERA, a provider of global market and economic information.



The team's estimates were an instrumental part of the comprehensive assessment of Barnett Shale reserves funded by the Alfred P. Sloan Foundation and issued earlier this year by the Bureau of Economic Geology at UT Austin.

Until now, estimates of shale gas production have primarily relied on models established for conventional oil and gas wells, which behave differently from the horizontal wells in gas-rich shales.

The researchers estimate the ultimate gas recovery from a sample of 8,294 horizontal wells in the Barnett Shale will be between 10 trillion and 20 trillion standard cubic feet (scf) during the lifetime of the wells. The study's well sample is made up of about half of the 15,000 existing wells in the Barnett Shale, the geological formation outside Fort Worth that offers the longest production history for hydrofractured horizontal wells in the world.

"With our model at hand, you can better predict how much gas volume is left and how long it will take until that volume will be depleted," Patzek said. "We are able to match historical production and predict future production of thousands of horizontal gas wells using this scaling theory."

"The contributions of shale gas to the U.S. economy are so enormous that even small corrections to production estimates are of great practical significance," Patzek said.

The researchers were surprised by how all of the wells they analyzed adhere to that simple scaling curve.

"By analyzing the basic physics underlying gas recovery from hydrofractured wells, we calculated a single curve that should describe how much gas comes out over time, and we showed that production from thousands of wells follows this curve," Marder said.

Patzek adds: "We are able to predict when the decline will begin. Once decline sets in, gas production goes down rapidly."

The decline of a well happens because of a process called pressure diffusion that causes pressure around a well to drop and gas production to decrease. The time at which gas pressure drops below its initial value everywhere in the rock between hydrofractures is called its interference time. On average, it takes five years for interference to occur, at which point wells produce gas at a far lower rate because the amount of gas coming out over time is proportional to the amount of gas remaining.

Using two parameters — a well's interference time and the original gas in place — the researchers were able to determine the universal decline curve and extrapolate total gas production over time.

The researchers found that the scaling theory accurately predicted the behavior of approximately 2,000 wells in which production had begun to decrease exponentially within the past 10 years. The remaining wells were too young for the model to predict when decreases would set in, but the model enabled the researchers to estimate upper and lower production limits for well lifetime and the amount of gas that will be produced by the wells.

Read more : http://www.geologypage.com/2013/11/ut-researchers-use-simple-scaling.html#ixzz2mXeoFR7b
 

Playa

Playa, ( Spanish: shore or beach) , also called pan, flat, or dry lake,  flat-bottom depression found in interior desert basins and adjacent to coasts within arid and semiarid regions, periodically covered by water that slowly filtrates into the ground water system or evaporates into the atmosphere, causing the deposition of salt, sand, and mud along the bottom and around the edges of the depression.

Playas are among the flattest known landforms. Their slopes are generally less than 0.2 metre per kilometre. When filled with only a few centimetres of water, many kilometres of surface may be inundated. It is the process of inundation that develops and maintains the near-perfect flatness so characteristic of these arid-region landforms.

Playas occupy the flat central basins of desert plains. They require interior drainage to a zone where evaporation greatly exceeds inflow. When flooded, a playa lake forms where fine-grained sediment and salts concentrate. Terminology is quite confused for playas because of many local names. A saline playa may be called a salt flat, salt marsh, salada, salar, salt pan, alkali flat, or salina. A salt-free playa may be termed a clay pan, hardpan, dry lake bed, or alkali flat. In Australia and South Africa small playas are generally referred to as pans. The low-relief plains of these lands contrast with the mountainous deserts of North America, resulting in numerous small pans instead of immense playas. The terms takyr, sabkha, and kavir are applied in Central Asia, Saudi Arabia, and Iran, respectively.

Saline flats are specialized forms located adjacent to large bodies of water, as, for example, along coasts, lakeshores, and deltas. They flood during storms, either with surface runoff or with surges from the nearby body of water. The saline crusts of saline flats are quite similar to those that develop in playas.

Role of flooding and groundwater

Playas affected by occasional surface floods are usually dry. Their surfaces consist of silt and clay deposited by the floodwaters that enter closed basins during the occasional flow events. Salts develop as ponded floodwater in the centre of such a basin gradually evaporates. Water also can be supplied to closed basins by groundwater flow. In basins dominated by groundwater inputs, sediment influxes are minimized, and saline crusts dominate. Moist areas may persist as groundwater flows to the lowest portion of playas. Very large playas may exhibit dry, sediment-dominated sections and moist, salt-dominated sections.

Physical characteristics

Enclosed basins of salt and clay accumulation may originate from numerous causes. Tectonic causes include faulting, as in the East African Rift Valley and Death Valley, and warping, as in Lake Eyre in Australia, Lake Chad in central Africa, and Shaṭṭ al-Jarīd (Chott Djerid) in Tunisia. Wind deflation can produce shallow basins with downwind dunes, as in southeastern Australia. Even very large basins, such as the Qattara Depression of Egypt, have been ascribed to deflation. Local cataclysmic disruptions of drainage (e.g., volcanism, landslides, and meteorite impacts) may produce playas in desert regions.

Modern playa surfaces are not passive receptors of sediment as they were once believed to be. They serve as important sources of dust and salts, which are blown to the surrounding uplands. Complex assemblages of minerals and sediments occur on the playa surfaces. These directly reflect their environment of deposition and may be used to interpret ancient environmental conditions.

Two broad classes of playas may be defined on the basis of past histories. One type develops from the desiccation of a former lake. Sediments in such a playa are primarily lacustrine, rather than derived from modern depositional processes. The second type of playa has no paleolacustrine heritage. Small salt pans in South Africa, called vokils, are of this type.

The supply of material, basin depth, and duration of accumulation all contribute to variations in the thickness of playa deposits. Very thick playa sequences may have alternating layers of lacustrine clays and salt beds. The former generally reflect periods of high floodwater runoff into the closed basins, perhaps induced by higher rainfall (so-called pluvial periods). Saline sediments or pure evaporite beds reflect arid climatic phases. The precise climatic interpretation of paleolacustrine playa sequences, however, can be problematic.



Read more : http://www.geologypage.com/2013/07/playa.html#ixzz2mXc8vQgO 

 

Constructor Oil and Gas Platforms Open Recruitment 2013 : Various Positions


PT GUNANUSA UTAMA FABRICATORS is a leading constructor oil and gas platforms in Indonesia. The company was established in 1983. To date, the company has successfully completed more than 100 offshore structures such as production, compression, wellhead, platforms/modules and jackets.

Our major clients are Total, BP, Caltex/UNOCAL/Chevron, Kodeko, MAXUS, Conoco-phillips, Hess, Etc. Our health, safety and environment (HSE management system conforms to the stringent requirement of all our clients and we have also obtain certification for ISO 9001 : 2000, ISO 14001 – 2004, and OHSAS 18001 – 2007. The company is also certified for U, U2, and S Stamps for the manufacture of pressure vessels and boilers.

Currently we are heading for several project, We are searching the best people for:

1. Entry Level (1-3 years experiences) (Jakarta / project)

a. Piping Engineer
b. Mechanical Engineer
c. Electrical Engineer
d. Civil Engineer
e. Buyer (piping and Mechanical
f. Material Control
g. Material Engineer
h. Contract Engineer
i. HR
j. Instrument engineer
k. Task sheet planner
l. Telecom Engineer
m. Marine officer
n. Offshore HSE officer
o. Structural Engineer
p. Project Cost Control

2. Mid-Level Pro-hire (5 – 9 years Experiences) (Jakarta / project)

a. Electrician precomm / comm.
b. Hook up Engineer
c. HSE Coordinator
d. TRA Coordinator
e. Instrument commissioning
f. NDE Coordinator
g. Piping Inspector
h. Piping Precomm/comm.

3. Senior-Level Pro-hire (10 up years experiences) (Jakarta)

a. QC Corporate Manager
b. Sr. Electrical Engineer
c. Sr. Mechanical Engineer
d. Risk management Manager
e. Sr. Instrument Manager
f. Sr. Naval Engineer
g. Sr. Structural Engineer
h. Sr. Welding Engineer

General Qualification:
1. High Motivated person
2. Have experience minimum in the category with offshore experience.
3. Want to placed onshore and offshore in all over Indonesia (based on project)
4. Fluent in English both Written and speaking
5. Good working on team
6. Have a leadership skill

Please send us your comprehensive CV with your updated photograph and EXPECTED SALARY by WORD / PDF format (not RAR format) with name position as SUBJECT.To; hrd@gunanusa.co.id
cc; resya.sujana@gunanusa.co.id
source :  http://oilandcareers.com/?p=2832

 

Western Indian Ocean Earthquake and Tsunami Hazard Potential Greater Than Previously Thought





Earthquakes similar in magnitude to the 2004 Sumatra earthquake could occur in an area beneath the Arabian Sea at the Makran subduction zone, according to recent research published in Geophysical Research Letters.
The research was carried out by scientists from the University of Southampton based at the National Oceanography Centre Southampton (NOCS), and the Pacific Geoscience Centre, Natural Resources Canada.
The study suggests that the risk from undersea earthquakes and associated tsunami in this area of the
Western Indian Ocean -- which could threaten the coastlines of Pakistan, Iran, Oman, India and potentially further afield -- has been previously underestimated. The results highlight the need for further investigation of pre-historic earthquakes and should be fed into hazard assessment and planning for the region.
Subduction zones are areas where two of Earth's tectonic plates collide and one is pushed beneath the other. When an earthquake occurs here, the seabed moves horizontally and vertically as the pressure is released, displacing large volumes of water that can result in a tsunami.

Plate boundary faults at subduction zones are expected to be prone to rupture generating earthquakes at temperatures of between 150 and 450 °C. The scientists used this relationship to map out the area of the potential fault rupture zone beneath the Makran by calculating the temperatures where the plates meet. Larger fault rupture zones result in larger magnitude earthquakes.


"Thermal modelling suggests that the potential earthquake rupture zone extends a long way northward, to a width of up to 350 kilometres which is unusually wide relative to most other subduction zones," says Gemma Smith, lead author and PhD student at University of Southampton School of Ocean and Earth Science, which is based at NOCS.

The team also found that the thickness of the sediment on the subducting plate could be a contributing factor to the magnitude of an earthquake and tsunami there.

"If the sediments between the plates are too weak then they might not be strong enough to allow the strain between the two plates to build up," says Smith. "But here we see much thicker sediments than usual, which means the deeper sediments will be more compressed and warmer. The heat and pressure make the sediments stronger. This results in the shallowest part of the subduction zone fault being potentially capable of slipping during an earthquake.

"These combined factors mean the Makran subduction zone is potentially capable of producing major earthquakes, up to magnitude 8.7-9.2. Past assumptions may have significantly underestimated the earthquake and tsunami hazard in this region.




see more : http://www.geologypage.com/2013/05/western-indian-ocean-earthquake-and.html
 

JOB OPPORTUNITY AT BP 2014



BP‘s business in Indonesia revolves around liquefied natural gas (LNG). Started in 2009, Tangguh is the first, fully integrated, end-to-end LNG operation in Indonesia, producing gas from Papua Barat offshore and delivering LNG to customers around Asia and the US. The Tangguh Expansion project involves the phased offshore development of platforms, new pipelines, a new 3.8mpta LNG train with a new integrated onshore receiving facility and new development wells.


As a high-reliability LNG producer, we are committed to safety and excellence in everything we do at Tangguh. Many talented upstream professionals have already joined us — but as the expansion gathers momentum, we can offer many more exciting opportunities to grow with the project in areas including:

- DEPUTY ENGINEERING MGR
- ELECTRICAL ENGINEER
- ENGINEERING TEAM LEAD GPF & PIPELINES
- CORROSION ENG
- DEPUTY ENGINEERING MGR
- INTEGRATED PLANNING TL
- SR. CONSTRUCTION ENG
- PROCESS SAFETY ENGINEER
- PROJECT OPERATIONS LEAD
- INTEGRATED PLANNING TL
- CAMP & PERMANENT BUILDING TL
- EARLY WORKS PROJECT TL
- OPERATION ENG
- FLOW ASSURANCE ENGINEER
- DCS TECHNICIAN

To find out more about these opportunities and apply visit bp.com/careers/indonesia

Discover BP
bp.com/careers/indonesia
BP is an equal opportunities employer
 

BP Andrew



BP Andrew - AAD Project taken by Mariusz Nieznanski -The quality of pictures just keeps getting better. Be sure to send yours to Petroleum Companies We will be running a competition before the end of the year to find your favourite picture of 2013.




 

National Museum of Natural History


The National Museum of Natural History is a natural history museum administered by the Smithsonian Institution, located on the National Mall in Washington, D.C., United States. With free admission and open doors 364 days a year, it is the most visited natural history museum in the world. Opened in 1910, the museum on the National Mall was one of the first Smithsonian buildings constructed exclusively to hold the national collections and research facilities. The main building has an overall area of 1,320,000 square feet (123,000 m2) with 350,000 square feet (33,000 m2) of exhibition and public space and houses over 1,000 employees.
The museum's collections total over 126 million specimens of plants, animals, fossils, minerals, rocks, meteorites, and humancultural artifacts. With 7.4 million visitors in 2009, it is the most visited of all of the Smithsonian museums that year and is also home to about 185 professional natural history scientists — the largest group of scientists dedicated to the study of natural and cultural history in the world.

Panoramic Virtual Tour

This comprehensive virtual tour allows visitors using a desktop computer (Windows, Mac, Linux) or a mobile device (iPhone, iPad, Android) to take a virtual, self-guided, room-by-room walking tour of the whole museum. You can even browse a list of past exhibits, which is included on the ground floor map (see upper right map buttons). The visitor can navigate from room to room by clicking map locations or by following blue arrow links on the floor that connect the rooms. The desktop version includes camera icons to indicate hotspots where the visitor can get a close-up view of a particular object or exhibit panel.

IN THIS LINK , YOU WILL SEE THING , YOU DON'T SEE IT BEFORE THIS MOMENT

http://www.mnh.si.edu/vtp/1-desktop/











 

700 Ton Ship Flips And Stands Upright In The Ocean - Amazing !!

700 Ton Ship Flips And Stands Upright In The Ocean - Amazing !!

The video features a very special type of ship that functions as an open ocean research vessel owned by the Office of Naval Research and operated by the Marine Physical Laboratory of the Scripps Institution of Oceanography. The 335 foot long vessel can flip upright and seemingly stand in the water in order to conduct research concerning wave science. RV FLIP (FLoating Instrument Platform) is an open ocean research vessel owned by the Office of Naval Research and operated by the Marine Physical Laboratory of the Scripps Institution of Oceanography.The ship is a 355 feet (108 meters) long vessel designed to partially flood and pitch backward 90 degrees, resulting in only the front 55 feet (17 meters) of the vessel pointing up out of the water, with bulkheads becoming decks. When flipped, most of the buoyancy for the platform is provided by water at depths below the influence of surface waves, hence FLIP is a stable platform mostly immune to wave action, like a spar buoy. At the end of a mission, compressed air is pumped into the ballast tanks in the flooded section and the vessel returns to its horizontal position so it can be towed to a new location.The ship is frequently mistaken for a capsized ocean transport ship FLIP is designed to study wave height, acoustic signals, water temperature and density, and for the collection of meteorological data. Because of the potential interference with the acoustic instruments, FLIP has no engines or other means of propulsion. It must be towed to open water, where it drifts freely or is anchored. In tow, FLIP can reach speeds of 7--10 knots. FLIP weighs 700 long tons (711 tonnes) and carries a crew of five, plus up to eleven scientists. It is capable of operating independently during month-long missions without resupply,being able to operate worldwide but the normal area is the west coast of the United States. The vessel operates out of a home base at the Scripps Nimitz Marine Facility in San Diego, California.


 

Chevron finds leak in offshore Petrobras oil field


U.S. oil company Chevron discovered an oil seep in an offshore Brazilian oil field run by Petrobras near the site of a November leak that led to civil and criminal charges and sparked concerns about some of the world's most promising deep sea reserves.No traces have been found on the surface, but droplets of oil were found leaking from the seabed of Petrobras' Roncador field, 500 meters away from Chevron's adjacent Frade field, Brazilian regulator ANP said.Chevron said it first detected the seep on Saturday.Leaks in November and March at Frade led to the suspension of operations there, as well as lawsuits for more than $20 billion and criminal charges against Chevron and its drilling contractor Transocean.
The Campos basin, which includes Roncador and Frade, and the neighboring Santos basin contain an estimated 100 billion barrels of oil. Brazil hopes the region will help it produce more than 7 million barrels a day of oil by 2020, passing the United States to be the world's No. 3 oil producer.Evidence of another leak in the basin quickly caught the attention of the prosecutor pressing charges against Chevron, who has already said he is expanding his investigation to other companies and fields in the Campos basin."I'm going to look at this very carefully," said Eduardo Santos de Oliveira by telephone. "It's very close to Frade."Still, some scientists have called the accusations swirling around the Campos basin hasty and exaggerated, in light of the small, naturally occurring seeps that originally attracted oil companies to the deep-sea deposits."We've confused things with the recent court cases," said geologist Cleveland Jones, of the State University of Rio de Janeiro, by telephone. "Seeps are common in the Campos Basin ... and oil in small amounts is not an ecological problem."PETROBRAS CONFIRMATIONChevron said it traced the seep with a remote submarine outside the Frade field."Upon further investigation with a remote operated vehicle, we determined the seep point was outside the boundary of the Frade field," Chevron said in a statement. "We have notified the operator of the concession."State-run Petrobras confirmed in a statement it had found the source of the oil seep in the seabed of its Roncador field, 120 kilometers (75 miles) off the coast of Rio de Janeiro.A November accident at a well in the Frade field caused a spill of about 3,000 barrels due to operational and safety violations and improper well design, according to the ANP's four-month investigation.Chevron's November spill was less than 0.1 percent the size of BP's 2010 Deepwater Horizon disaster in the Gulf of Mexico. In the BP spill, 11 died and about 4.9 million barrels leaked over three months. In Frade, no one was hurt, no oil came near the Brazilian coast and the leak was stopped in four days, according to Chevron.The subsequent March seep in the Frade field led Chevron and its partners there, Petrobras and a Japanese group led by Inpex and Sojitz, to shut down production at the field, which was averaging 62,000 barrels daily, in order to study the source of the leak.Chevron said the March leak totaled about two barrels, over half of which was captured, making it less than 0.1 percent of the field's November spill.




Source: Reuters http://egyptoil-gas.com/read_article_international.php?NID=2451

 

GDF SUEZ signs an agreement with Sempra Energyto access natural gas liquefaction capacity in the United States



...

GDF SUEZ announces the signature of a commercial development agreement with Cameron LNG, a unit of Sempra Energy, regarding the natural gas liquefaction project of Cameron LNG in the United States. This facility will be located at the site of its existing import terminal located in Hackberry, Louisiana. Through this commercial development agreement, GDF SUEZ and Sempra will negotiate a 20 year liquefaction service contract for 4 million tons per annum (MTPA) of liquefied natural gas (LNG).


The LNG plant will have 3 liquefaction trains with a production and export capacity of 12 MTPA and will be operated by Cameron LNG. This new LNG plant is expected to start full operations in late 2016.


Jean-Marie Dauger, Executive Vice-President of GDF SUEZ in charge of the Global Gas & LNG business line commented: “Accessing new LNG volumes from United States will contribute to grow and further diversify GDF SUEZ LNG portfolio and is consistent with its leadership in the LNG sector. This new LNG supply source will reinforce the flexibility and the security of supply of GDF SUEZ’ natural gas portfolio. It will be a step further toward satisfying the LNG import requirements in our current markets, especially in Europe, and will also support the development of new international markets for GDF SUEZ”.


Sempra Energy operates two LNG regasification terminals in North America (Energia Costa Azul near Ensenada in Mexico and Cameron LNG in the US).


GDF SUEZ is one of the leading LNG players in the world and the main LNG importer in Europe. Its LNG portfolio of 16.5 MTPA, sourced from 6 countries, is the third largest in the world. .

 
 
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