Ulcerative colitis(UC)is a chronic,nonspecific,relapsing inflammatory bowel disease.The colorectum is considered the chief target organ of UC,whereas upper gastrointestinal(UGI)tract manifestations are infrequent.Rece...Ulcerative colitis(UC)is a chronic,nonspecific,relapsing inflammatory bowel disease.The colorectum is considered the chief target organ of UC,whereas upper gastrointestinal(UGI)tract manifestations are infrequent.Recently,emerging evidence has suggested that UC presents complications in esophageal,stomachic,and duodenal mucosal injuries.However,UC-related UGI tract manifestations are varied and frequently silenced or concealed.Moreover,the endoscopic and microscopic characteristics of UGI tract complicated with UC are nonspecific.Therefore,UGI involvement may be ignored by many clinicians.In addition,no standard criteria have been established for patients with UC who should undergo fibrogastroduodenoscopy.Furthermore,specific treatment recommendations may be needed for patients with UC-associated UGI lesions.Herein,we review the esophageal,gastric,and duodenal mucosal lesions of the UC-associated UGI tract,as well as the potential pathogenesis and therapy.展开更多
In order to study the deterioration characteristics of the microscopic structure of sandstones in freeze-thaw cycles, tests of180 freeze-thaw cycles were performed on sandstone specimens. The nuclear magnetic resonan...In order to study the deterioration characteristics of the microscopic structure of sandstones in freeze-thaw cycles, tests of180 freeze-thaw cycles were performed on sandstone specimens. The nuclear magnetic resonance （NMR） technique was applied tothe measurement of sandstone specimens and analysis of the magnetic resonance imaging. Then, the fractal theory was employed tocompute the fractal dimension values of pore development of rocks after different freeze-thaw cycles. The results show that the massand porosity of rocks grow with the increase of freeze-thaw cycles. According to the NMR T2 distribution of sandstones, the poresizes of rock specimens increase after 180 freeze-thaw cycles, especially that of the medium-sized and small-sized pores. The spatialdistribution of sandstone pores after freeze-thaw cycles has fractal features within certain range, and the fractal dimension ofsandstones tends to increase gradually.展开更多
Coal and gas outburst is a frequent dynamic disaster during underground coal mining activities.After about 150 years of exploration,the mechanisms of outbursts remain unclear to date.Studies on outburst mechanisms wor...Coal and gas outburst is a frequent dynamic disaster during underground coal mining activities.After about 150 years of exploration,the mechanisms of outbursts remain unclear to date.Studies on outburst mechanisms worldwide focused on the physicochemical and mechanical properties of outburst-prone coal,laboratory-scale outburst experiments and numerical modeling,mine-site investigations,and doctrines of outburst mechanisms.Outburst mechanisms are divided into two categories:single-factor and multi-factor mechanisms.The multi-factor mechanism is widely accepted,but all statistical phenomena during a single outburst cannot be explained using present knowledge.Additional topics about outburst mechanisms are proposed by summarizing the phenomena that need precise explanation.The most appealing research is the microscopic process of the interaction between coal and gas.Modern physical-chemical methods can help characterize the natural properties of outburst-prone coal.Outburst experiments can compensate for the deficiency of first-hand observation at the scene.Restoring the original outburst scene by constructing a geomechanical model or numerical model and reproducing the entire outburst process based on mining environment conditions,including stratigraphic distribution,gas occurrence,and geological structure,are important.Future studies can explore outburst mechanisms at the microscale.展开更多
文摘Ulcerative colitis(UC)is a chronic,nonspecific,relapsing inflammatory bowel disease.The colorectum is considered the chief target organ of UC,whereas upper gastrointestinal(UGI)tract manifestations are infrequent.Recently,emerging evidence has suggested that UC presents complications in esophageal,stomachic,and duodenal mucosal injuries.However,UC-related UGI tract manifestations are varied and frequently silenced or concealed.Moreover,the endoscopic and microscopic characteristics of UGI tract complicated with UC are nonspecific.Therefore,UGI involvement may be ignored by many clinicians.In addition,no standard criteria have been established for patients with UC who should undergo fibrogastroduodenoscopy.Furthermore,specific treatment recommendations may be needed for patients with UC-associated UGI lesions.Herein,we review the esophageal,gastric,and duodenal mucosal lesions of the UC-associated UGI tract,as well as the potential pathogenesis and therapy.
基金Projects(41502327,51474252)supported by the National Natural Science Foundation of ChinaProject(2013YQ17046310)supported by the National Key Scientific Instrument and Equipment Development Project of China+1 种基金Project(20130162120012)supported by the Special Research Fund for the Doctoral Program of Higher Education of ChinaProject(2015CX005)supported by Innovation Driven Plan of Central South University,China
文摘In order to study the deterioration characteristics of the microscopic structure of sandstones in freeze-thaw cycles, tests of180 freeze-thaw cycles were performed on sandstone specimens. The nuclear magnetic resonance （NMR） technique was applied tothe measurement of sandstone specimens and analysis of the magnetic resonance imaging. Then, the fractal theory was employed tocompute the fractal dimension values of pore development of rocks after different freeze-thaw cycles. The results show that the massand porosity of rocks grow with the increase of freeze-thaw cycles. According to the NMR T2 distribution of sandstones, the poresizes of rock specimens increase after 180 freeze-thaw cycles, especially that of the medium-sized and small-sized pores. The spatialdistribution of sandstone pores after freeze-thaw cycles has fractal features within certain range, and the fractal dimension ofsandstones tends to increase gradually.
基金financially supported by the State Key Research Development Program of China(No.2016YFC0600708)the Fundamental Research Funds for the Central Universities(No.2009kz03)+1 种基金the Scientific and Technological Innovation Leading Talents of“Ten thousand plan”of the Organization Department of the Central Committee of the CPC(No.W02020049)the International Clean Energy Talent Program of State Scholarship Fund of China Scholarship Council(No.201902720011)。
文摘Coal and gas outburst is a frequent dynamic disaster during underground coal mining activities.After about 150 years of exploration,the mechanisms of outbursts remain unclear to date.Studies on outburst mechanisms worldwide focused on the physicochemical and mechanical properties of outburst-prone coal,laboratory-scale outburst experiments and numerical modeling,mine-site investigations,and doctrines of outburst mechanisms.Outburst mechanisms are divided into two categories:single-factor and multi-factor mechanisms.The multi-factor mechanism is widely accepted,but all statistical phenomena during a single outburst cannot be explained using present knowledge.Additional topics about outburst mechanisms are proposed by summarizing the phenomena that need precise explanation.The most appealing research is the microscopic process of the interaction between coal and gas.Modern physical-chemical methods can help characterize the natural properties of outburst-prone coal.Outburst experiments can compensate for the deficiency of first-hand observation at the scene.Restoring the original outburst scene by constructing a geomechanical model or numerical model and reproducing the entire outburst process based on mining environment conditions,including stratigraphic distribution,gas occurrence,and geological structure,are important.Future studies can explore outburst mechanisms at the microscale.
