New York, Jan 3, 2018: Providing safer drinking water to those in need may become a little easier as researchers have developed a new desalination technique that removes salt from water using less energy than previous methods.
“Globally, there is reduced access to fresh water,” said one of the researchers Bruce Logan, Professor at Pennsylvania State University in the US.
“More and more, the waters that are being used are impaired, either due to salt or other contaminants, so we are seeing an increasing need to rely on less optimal water sources,” Logan said.
With an aim to combat this problem, Logan and his colleagues came up with a desalination method called battery electrode deionization (BDI).
Although the current configuration is not suited to desalinate extremely salty water such as seawater, the results, published in the journal Environmental Science & Technology Letters, showed that the BDI technique could be effective as a low energy method for brackish, or slightly salty, water, such as groundwater, or for desalinating water before it enters treatment plants.
“There is nothing that inherently prevents its use with seawater, it’s just that as water gets saltier and saltier, there are other issues that we have to contend with, such as increased energy consumption and membrane fouling, that may reduce its utility relative to other approaches,” Logan said.
The new method improves upon standard capacitive deionisation techniques by eliminating the regeneration stage and lowering the voltage required to complete the process, the study said. (IANS)
Mars once had salt lakes similar to the ones on Earth and has gone through wet and dry periods, according to a new study.
The researchers from Texas A&M University College in the US examined Mars’ geological terrains from Gale Crater, an immense 95-mile-wide rocky basin that is being explored by the NASA Curiosity rover since 2012 as part of the MSL (Mars Science Laboratory) mission, according to the study published in the journal Nature Geoscience.
The results show that the lake, which was present in Gale Crater over three billion years ago underwent a drying episode, potentially linked to the global drying of Mars.
Gale Crater was formed about 3.6 billion years ago when a meteor hit Mars.
“Since then, its geological terrains have recorded the history of Mars, and studies have shown Gale Crater reveals signs that liquid water was present over its history, which is a key ingredient of microbial life as we know it,” said study co-author Marion Nachon from Texas A&M University.
“During these drying periods, salt ponds eventually formed. It is difficult to say exactly how large these ponds were, but the lake in Gale Crater was present for long periods of time – from at least hundreds of years to perhaps tens of thousands of years,” Nachon said.
According to the researchers, Mars probably became drier over time, and the planet lost its planetary magnetic field, which left the atmosphere exposed to be stripped by solar wind and radiation over millions of years.
“With the atmosphere becoming thinner, the pressure at the surface became lesser, and the conditions for liquid water to be stable at the surface were not fulfilled anymore, so liquid water became unsustainable and evaporated,” Nachon said.
The salt ponds on Mars are believed to be similar to some found on Earth, especially those in a region called Altiplano, which is near the Bolivia-Peru border.
Nachon said that the Altiplano is an arid, high-altitude plateau where rivers and streams from mountain ranges “do not flow to the sea but lead to closed basins, similar to what used to happen at Gale Crater on Mars.
“This hydrology creates lakes with water levels heavily influenced by climate. During the arid periods Altiplano lakes become shallow due to evaporation, and some even dry up entirely,” she said.
Nachon added that the study shows that the ancient lake in Gale Crater underwent at least one episode of drying before “recovering.”
It’s also possible that the lake was segmented into separate ponds, where some of the ponds could have undergone more evaporation.