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Objective: To investigate the protective effects of curcumin on bile duct ligation(BDL)-induced liver cholestasis in mice, so as to provide a new treatment strategy for liver fibrosis., Methods: Forty-two healthy adult male BALB/c mice were randomly divided into sham group (n =6), sham+curcumin group (n=6), BDL treatment group (n=10), BDL+curcumin group(n=10), BDL+curcumin+ZnPP group (n=10). Seven days after BDL operation, the sham operation + curcumin group and the BDL+ curcumin group were treated with curcumin at the dose of 30 mg/kg by intraperitoneal injection once a day for 7 days.The mice in BDL+ curcumin +ZnPP group were treated with curcumin (30 mg/kg) and ZnPP (50 μmol/kg) by intraperitoneal injection once a day for 7 days. For the sham group and the BDL group, mice were treated with equal-volume saline daily by intraperitoneal injection. After 14 days of BDL, the plasma and liver tissues were collected, the levels of aspartate aminotransferase (AST) and alanine aminotransferase (ALT) were measured. The pathological changes of liver tissue and liver fibrosis were observed, and the protein expression of HO-1 in liver tissue was detected., Results: Compared with the sham group, mice in the BDL group had enlarged liver gallbladder and the serum levels of ALT and AST were increased significantly (P＜0.05). Meanwhile, the results of Sirius red staining and qRT-PCR of pro-fibrosis related genes showed collagen deposition in the liver, and immunohistochemistry of macrophages and neutrophils showed inflammatory cell infiltration in the liver. Compared with the BDL group, the serum levels of ALT and AST in the curcumin treatment group were decreased significantly (P＜0.05), collagen deposition and inflammatory cell infiltration were improved, and HO-1 expression was increased (P＜0.05) after curcumin treatement. In the curcumin treatment group, the protective effect of curcumin on liver injury could be reversed by HO-1 active inhibitor ZnPP., Conclusion: Curcumin can improve liver inflammation and fibrosis caused by BDL, and this protective effect is related to the regulation of HO-1 activity by curcumin.

Passive microwave remote sensing offers its all-weather work capabilities, but atmospheric influences on satellite microwave brightness temperature were different under different atmospheric conditions and environments. In order to clarify atmospheric influences on Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E), atmospheric radiation were simulated based on AMSR-E configuration under clear sky and cloudy conditions, by using radiative transfer model and atmospheric conditions data. Results showed that atmospheric water vapor was the major factor for atmospheric radiation under clear sky condition. Atmospheric transmittances were almost above 0.98 at AMSR-E's low frequencies (< 18.7 GHz) and the microwave brightness temperature changes caused by atmosphere can be ignored in clear sky condition. Atmospheric transmittances at 36.5 and 89 GHz were 0.896 and 0.756 respectively. The effects of atmospheric water vapor needed to be corrected when using microwave high-frequency channels to inverse land surface parameters in clear sky condition. But under cloud cover or cloudy conditions, cloud liquid water was the key factor to cause atmospheric radiation. When sky was covered by typical stratus cloud, atmospheric transmittances at 10.7, 18.7 and 36.5 GHz were 0.942, 0.828 and 0.605 respectively. Comparing with the clear sky condition, the down-welling atmospheric radiation caused by cloud liquid water increased up to 75.365 K at 36.5 GHz. It showed that the atmospheric correction under different clouds covered condition was the primary work to improve the accuracy of land surface parameters inversion of passive microwave remote sensing. The results also provided the basis for microwave atmospheric correction algorithm development. Finally, the atmospheric sounding data was utilized to calculate the atmospheric transmittance of Hailaer Region, Inner Mongolia province, in July 2013. The results indicated that atmospheric transmittances were close to 1 at C-band and X-band. 89 GHz was greatly influenced by water vapor and its atmospheric transmittance was not more than 0.7. Atmospheric transmittances in Hailaer Region had a relatively stable value in summer, but had about 0.1 fluctuations with the local water vapor changes.

The microwave emissivity is a function of structure, water content, and surface roughness, and all these factors have obvious seasonal variations. In the present study, the half-month averaged emissivities in summer and winter of 2003 over the vegetation of Northern Hemisphere were estimated using Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E) combined with IGBP (International Geosphere-Biosphere Project labels) land classification data. Then the emissivities of vegetation land covers at different frequencies, the polarization and their seasonal variations were analyzed respectively. The results show that the emissivities of vegetation increase with the increase in frequencies, and decline with the frequency increasing over snow region. In summer, the vegetation emissivity at V-polarization of 89 GHz is larger than 0.944, and all emissivities are relatively stable and the RMSE of time series emissivity variation is less than 0.007 2. In winter, emissivities decrease over snow covered area, especially for higher frequencies. Furthermore, with the increase in vegetation density, the emissivities increase and emissivity polarization difference decreases.

The microwave emissivity over land is very important for describing the characteristics of the lands, and it is also a key factor for retrieving the parameters of land and atmosphere. Different land covers have their emission behavior as a function of structure, water content, and surface roughness. In the present study the global land surface emissivities were calculated using six month (June, 2003-August, 2003, Dec, 2003-Feb, 2004) AMSR-E L2A brightness temperature, MODIS land surface temperature and the layered atmosphere temperature, and humidity and pressure profiles data retrieved from MODIS/Aqua under clear sky conditions. With the information of IGBP land cover types, "pure" pixels were used, which are defined when the fraction cover of each land type is larger than 85%. Then, the emissivity of sixteen land covers at different frequencies, polarization and their seasonal variation were analyzed respectively. The results show that the emissivity of vegetation including forests, grasslands and croplands is higher than that over bare soil, and the polarization difference of vegetation is smaller than that of bare soil. In summer, the emissivity of vegetation is relatively stable because it is in bloom, therefore the authors can use it as its emissivity in our microwave emissivity database over different land cover types. Furthermore, snow cover can heavily impact the change in land cover emissivity, especially in winter.