The gradient acquisition plots (Fig. 6; Kruiver et al. 2001) confirmed the presence of a component with a narrow coercivity range, around 40 mT, for which the intensity increased with water depth (Fig. 4).
The hydrothermal exotherm gained intensity with increasing water content, with the onset temperature remaining relatively constant, although the peak maximum was beyond the 220 °C limit of the sealed DSC cells.
The efficiency of the system was observed directly related with insulation thickness and solar intensity and inversely with water depth.
On the other hand, the isotopic effect on the accumulation of spin adducts is clearly seen; i.e., the DMPO OH spectra intensity in water with composition of 40.7% (O) H2O + 57.7% (O) H2O is less than in 100% O water (lines 2 and 1 in Figure 1, respectively).
During the rainstorms, some runoff rates on the loess slopes with thicker sand layers were higher than the rainfall intensity due to rainwater combining with water emerging from the saturated sand, which could never occur on the uncovered loess slope.
The intensity of absorption bands associated with water increased with the CsCl amount, confirming the hygroscopicity of CsCl.
The intensity of absorption bands associated with water increase with the CsCl amount, confirming the hygroscopicity of CsCl [16].
For a given alkali, the intensity of this peak changes with water content, but not its shape.
One of the most notable elements of fracking that continues to be shrouded in secrecy, for instance, is the identity and mixture of chemicals that are injected into the ground through wells, together with water, at high intensity to fracture underground rocks and release oil or gas.
The PBS was replaced with water and fluorescence intensity of DiI was measured for each well at 549 nm excitation and 565 nm emission wavelengths using a SAFIRE fluorescent microplate reader (Tecan US Inc., Durham, NC, USA).
