Scientists from Tsinghua University took
samples from surface water the industrial wastewater, in the municipal wastewater treatment plant, and from Ouijang River, at Wenzhou city, which receives the treated wastewater.
Not exact matches
The next step will be to
sample the lunar
surface, finding ways to build with it or extract resources (especially
water)
from it.
But recently, NASA spacecraft and new research on
samples from the Apollo missions have shown that the moon actually has
water, both on and beneath its
surface.
Even with advances in drillingtechniques, it is difficult to obtain
samples from wells that have notbeen contaminated by air or
water from the
surface.
But recently, NASA spacecraft and new research on
samples from the Apollo missions have shown that the Moon actually has
water, both on its
surface and beneath.
It also would be far easier to get a
water sample from Enceladus, which has plumes of
water vapor, ice and particles shooting more than 300 miles off its
surface, than
from other moons, such as Jupiter's Europa, where a massive ocean is believed to be buried beneath a thick icy crust.
Research cruises such as Tara Oceans and the Global Ocean
Sampling Expedition have begun to
sample, sequence and analyze the ocean microbiome,
from the sunlit
surface waters that are mixed by the wind to dark deep layers that relatively unperturbed.
It is widely realized that WWii saw changes in the construction of
sampling buckets for sea
surface temperature measurement, and many navies switching to
water intake temperatures in compiling data
from ships at sea.
The areas where
water samples drawn
from near -
surface layers had traces of the natural contaminants
from the deep shale layers showed no relationship to past or current gas drilling activity, the researchers reported.
(B)
Surface water temperatures (means ± s.d.)
from the predominantly freshwater
sampling sites in the San Francisco Estuary / Sacramento — San Joaquin Rivers Delta system, California, USA.
Most interesting is that the about monthly variations correlate with the lunar phases (peak on full moon) The Helsinki Background measurements 1935 The first background measurements in history;
sampling data in vertical profile every 50 - 100m up to 1,5 km; 364 ppm underthe clouds and above Haldane measurements at the Scottish coast 370 ppmCO2 in winds
from the sea; 355 ppm in air
from the land Wattenberg measurements in the southern Atlantic ocean 1925-1927 310
sampling stations along the latitudes of the southern Atlantic oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the sea; high ocean outgassing crossing the warm
water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936
sampling CO2 over sea
surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic
from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2
sampling on swedish island (Kattegatt) in summer
from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly average
Striking changes in salinity are found
from the
surface to the bottom in the northern North Atlantic near
water mass formation sites that fill the
water column (Section 5.3.2); bottom changes elsewhere are small, being most prevalent at the under -
sampled southern ends of both sections.
The research team, including the authors of the study, Peter Davison and Rebecca Asch, traveled across hundreds of miles of the North Pacific ocean gyre, collecting fish specimens,
water samples and marine debris at depths ranging
from the
surface to thousands of feet under.
However, because extra energy warmth
surface water, you would require to take
water samples from below to really understand the entire situation.