The experimental results and security analyses demonstrate that the proposed method has a fine security performance.
These analyses demonstrate that the Caty_1.0 reference genome is of sufficient quality to facilitate population-scale whole-genome and transcriptome sequencing studies.
The analyses demonstrate that the effects of the drivers differ substantially with regard to the investigated aspects of innovation.
X-ray diffraction, Raman spectrum, and transmission electron microscopic analyses demonstrate that the product is single-crystalline Fe3O4.
The results from both of the analyses demonstrate that the equation is reasonable and has satisfactory accuracy to an extent.
Our petrological analyses demonstrate that the magma erupted as pumice from the Plinian eruptions in 1914, 1779, and 1471 was stored in the shallow conduit, not in the main reservoir ~10 km beneath the Aira caldera.
The analyses demonstrate that the physical mechanisms involved are associated with an additional circulation caused by the fluid viscosity and with the Venturi effect.
Furthermore, deletion analyses demonstrate that the C-terminal 41 amino acids of v=MybAMV (amino acids 331 to 371 of the Myb portion) are nonessential whereas further deletion of amino acids 321 to 330 (EFAETLQLID) results in a nonfunctional protein.
The results and analyses demonstrate that the proposed optical cryptography network topologies possess high security, and a new research perspective may be opened up for optical image encryption.
Finally, theoretical and experimental analyses demonstrate that the proposed technique can effectively resist different types of malicious reconnaissance strategies and ensure low mutation overhead at the same time.
The data analyses demonstrate that the constitutive equations derived in Part I provide an excellent phenomenological representation of the interactive creep and swelling phenomena.
