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Background & Objective:With the aggravation of global aging, benign prostate hyperplasia tends to have a higher incidence and has been the most common disease in urinary surgery. It is usually treated by surgery. Our objective was to select an effective treatment scheme, the clinical efficacy and relevant indicators of transurethral balloon dilatation of the prostate (TUDP) and transurethral plasmakinetic resection of the prostate (PKRP) in the treatment of benign prostate hyperplasia were emphatically compared.Methods:Ninety-eight patients with benign prostate hyperplasia who were admitted to the hospital of between May 2014 and July 2016 were selected and divided into a TUDP group (n=49) and PKRP (n=49) using random number table. The intraoperative blood loss, duration of surgery, international prostate symptom score (IPSS), quality of life (QOL), post-void residual urine (PVR) and complications of the two groups were observed.Results:The results demonstrated that the postoperative blood loss and duration of surgery of the patients in the PKRP group were significantly higher than those of the TUDP group (P<0.05); the IPSS, QOL and PVR of the patients in the two groups after surgery were much lower than those before surgery (P<0.05); the IPSS, QOL and PVR of the patients in the PKRP group were significantly lower than those in the TUDP group after surgery (P<0.05). The incidence of postoperative complications of the PKRP group was 38.8%, which was apparently higher than 14.3% in the TUDP group (P<0.05).Conclusion:PKRP has better efficacy than TUDP in treating benign prostatic hyperplasia, but QOL was poor and there are many complications. Proper surgical procedure should be selected according to the specific disease condition of patients.

Pyrites are widely distributed in marine sediments, the morphology of which is applied as a proxy to infer the redox conditions of bottom water, and identify diagenetic stages and hydrocarbon leakage activities. In this review, the methods used for the morphological study of pyrite are summarized. The textural and size characteristics of euhedral pyrite and pyrite aggregates, as the formation and evolution mechanism of pyrite are discussed for their significance in reconstructing the geochemical environment. The morphological study of pyrite includes shape observation, size estimation, and surface feature analysis. Scanning electron microscope and optical microscope are the main methods for morphological observation; transmission electron microscope and scanning tunneling microscope are applicable to observe nanoscale morphological structures and crystal growth on the crystal surface, and X-ray computed tomography is capable of measuring pyrite size distribution at the scale of a micrometer. Under the marine sedimentary condition, the single crystal of pyrite appears in cube, octahedron, dodecahedron, and their intermediates, the size of which ranges from several nanometers to more than 100 µm. The morphology of euhedral pyrite is controlled by temperature, pH, the chemical composition of interstitial water, etc., and might have been experienced in later reformation processes. The pyrite aggregates occur as framboid, rod-like, fossil-infilling, etc., characterized by the comparatively large size of several microns to several millimeters. It is found that certain textures correspond with different formation mechanisms and geochemical environments. Particularly, under special geological conditions, for instance, the methane leakage and/or decomposition of gas hydrate, pyrite is anomaly enriched with morphological textures of massive framboid cluster, rod-like aggregates, etc., and framboid is found with a large mean diameter (>20 µm) and standard deviation (>10 µm). These typical features can be employed to ascertain the position of the paleo sulfate methane transition zone (SMTZ).

With more natural gas hydrate samples recovered and more research approaches applied to hydrate-associated gas studies, data concerning the geochemical characteristics of hydrate-associated gases have been increased significantly in the past decades. Although systematic reviews of hydrocarbons are available, fewer studies have focused on the systematic classification of gas hydrates, yet. In this study, the primary origins and secondary processes that affect the geochemical characteristics of the gases are discussed. The primary origins are affected mainly by the type and /or maturity of the organic matter, which determine the main signature of the gas is microbial gas or thermogenic gas in a broad scheme. Apart from primary origins, secondary processes after gas generation such as migration, mixing, biodegradation and oxidation occur during the migration and/or storage of gases can significantly alter their primary features. Traditional methods such as stable isotope and molecular ratios are basic proxies, which have been widely adopted to identify these primary origins and secondary processes. Isotopic compositions of C2+ gases have been employed to identify the precursor of the gases or source rocks in recent years. Data from novel techniques such as methane clumped isotope and noble gases bring additional insights into the gas origins and sources by providing information about the formation temperature of methane or proxies of mantle contribution. A combination of these multiple geochemical approaches can help to elucidate an accurate delineation of the generation and accumulation processes of gases in a gas hydrate reservoir.