Because of RO's unique abilities, there is growing
interest in implementing membrane processes for treating salty groundwater
(brackish water), impaired rivers, and post-consumer reclaimed waters
in addition to producing fresh water from the world's most plentiful
water resource - our oceans. On average, seawater contains approximately
35,000 mg/L of salt, nearly two orders of magnitude
higher than that of potable water (United States
has a secondary standard of 500 mg/L). Brackish water has lower salinity
than seawater and ranges between 1,000-25,000 mg/L.
Use of desalination technology dates back to the ancient times, when
Greek sailors purified water by seawater evaporation. During
the middle of the twentieth century, desalination
technology became the primary source of fresh water supply in the arid
regions of the
world where water is in short supply. Conventionally,
thermal technologies (evaporative processes), which are energy intensive
and
costly approaches, have been employed for
desalination by oil-rich nations. The largest thermal based desalination
facility in the
world; Shoaiba (located in Saudi Arabia)
began operating in 2003 and has a production capacity of 93 MGD.
Recent advancements in membrane technologies along with energy recovery
systems have made RO, and possibly nanofiltration, a more cost effective
approach to desalination. These membrane technologies use high pressure
to force water through semi-permeable
membranes, which in turn, retain dissolved
and suspended solids. The largest RO facility in the world is located
in Ashkelon,
Israel and began operating in 2006 with a production capacity
of 73 MGD. The first large-scale seawater RO desalination plant in the
U.S. began operations in Tampa,
Florida, early in 2004. Worldwide, there
are over 21,000 desalination plants (in more than 120 countries) producing
more than 10.5 billion gallons of potable water a day. Following table
summarizes a list of key desalination facilities
around the world: |
It is estimated that 50% of the future
population growth in the United States will
occur in the coastal states of California, Florida, and Texas. Interestingly,
these three states are also the nation's leaders in seawater desalination.
In California, many water agencies are interested in reducing their
dependence on imported water and view seawater desalination as a viable
local source of water. Currently, there are about a dozen small and
large size desalination plants in the coastal regions of California.
Proposals for more than two dozen additional seawater desalination plant
are under review; some of these proposed plants could be the largest
in the US and the western hemisphere.
In the past, prohibitive costs
restricted widespread applications of desalination
technology and conventional treatment of
traditional water sources (groundwater, surface water and out-of-state
transfers) was more cost effective. Increasing population, industrialization,
frequent and prolonged droughts, dwindling traditional sources, and
new stringent regulations are continuously pushing the costs of the
conventional water supplies up, bringing seawater (and brackish water)
desalination back to the world stage.
Driven by advances in material
science, modern desalination membranes (such
as thin-film composite membranes) use much lower pressures to produce
a gallon of water than their predecessors.
Also, dramatic improvements in the design
of feed pumps and pressure exchangers have significantly reduced energy
costs, which is a significant economic advantage; as energy costs can
account for as much as one-half the total cost of the process. Additionally,
these modern membranes have better mechanical and chemical stability,
which results in longer life span than membranes produced just a decade
ago. Other significant forces, such as increasing desalination plant
capacity, co-location with power generation facilities, and the concept
of “built-operate-own-transfer”,
(which increases competition among the desalination
contractors), and new stringent regulations
are bridging the gap between cost of conventional water supplies and
desalinated water.
Today, water
desalination is a viable option for providing
high-quality drinking water that can meet, typically exceed, the most
stringent Federal drinking water quality standards. Although significant
institutional hurdles exist, desalination holds the key to a drought
proof, environmental friendly, and sustainable future potable water
supply.
Brackish water: Brackish water is characterized
by the presence of higher total dissolved solid (TDS) levels than potable
water, but lower TDS levels than seawater (in the range of 1,000 mg/l
TDS to 25,000 mg/l TDS). Brackish water can be found in the coastal
areas where fresh water mixes with the ocean (such as bays and estuaries),
in aquifers (where it is usually referred to as saline water), and
in surface waters (salt marshes, for instance, contain brackish water).
Conventional water treatment technologies:
Typical conventional water treatment consists of screening to remove
debris; coagulation to combine solids so that they settle; sedimentation
to settle suspended solids; and filtration. Conventional water treatment
processes have been around for more than 100 years.
Ground water: Water normally found underground
and obtained from wells. It should not be confused with surface water
such as rivers, ponds, lakes, or waters above the water table.
Sandia
National Laboratories and the U.S. Department of Interior, Bureau of Reclamation (2003),
Report #95, Desalination and Water Purification Technology Roadmap.
Water
Science and Technology Board (2004) Review of
the Desalination and Water Purification Technology Roadmap, The National
Academy Press.
California
Coastal Commission (2004) Seawater Desalination
and the California Coastal act.
Texas Water Development Board (2004) The Future
of Desalination in Texas Volume 1: Biennial Report
on Seawater Desalination.
Young,
M., Proctor, W., Qureshi E., and Wittwer, G.
(2006), Without Water: The economics of supplying water to 5 million
more Australians, Policy and Economic Research Unit, CSIRO Land and Water;
and Centre for Policy Studies, Monash University, Australia. |