以短肽组装体为模板仿生矿化二氧化硅纳米管

目的 二氧化硅纳米管由于具有生物相容性好、光学性质优异等特殊性能在不同领域展现出良好的应用前景，其尺寸和形貌可显著影响材料性质。为制备尺寸较大的纳米管并拓展其在不同领域的应用，本研究选择尺寸较大的多肽组装体为模板，进行二氧化硅的仿生矿化。方法 以Bola型多肽Ac-KI₃VK-CONH₂自组装形成的尺寸较大（直径约40 nm）的纳米管为模板，通过仿生矿化的方法制备二氧化硅纳米材料。首先考察了多肽纳米管的稳定性，发现在稀释、加入有机溶剂和改变溶液pH值时，纳米管的形貌均被破坏，展示出较差的稳定性。在此基础上，以该多肽纳米管为模板，选择反应速率较快的正硅酸甲酯（TMOS）为前驱体仿生矿化二氧化硅纳米材料，探索了不同矿化条件对二氧化硅纳米管尺寸和形貌的影响。结果 以反应速率较快的TMOS为硅源、体积百分比浓度为1.11%~3.33%、溶液为中性或者弱碱性时能够矿化形成形貌和尺寸较大且分布均匀的二氧化硅纳米管。结论 通过选择合适的多肽组装体模板和反应速率快的TMOS为硅源，成功制备出了尺寸较大的二氧化硅纳米管，这为拓展其在不同领域的应用奠定了基础，具有重要意义。     

INTAKES OF SELECTED NUTRIENTS,BONE MINERALISATION AND DENSITY OF ADOLESCENT FEMALE SWIMMERS OVER A THREE-YEAR PERIOD

The aim of this study was to conduct three-year monitoring of bone mineralization (BMC) and bone mineral density (BMD) of adolescent girls engaged in swimming at the time of attaining the peak bone mass and of their counterparts leading a rather sedentary life, considering the intakes of calcium, phosphorus and protein, as well as the proportions among those nutrients. Two groups of girls aged 11–13 years were studied 3 times at yearly intervals: untrained controls (n = 20) and those engaged in competitive swimming (n = 20). Bone density was determined by dual-energy X-ray absorptiometry (DXA) in the lumbar spine (L2 – L4). Nutrient intakes (energy, protein, calcium, phosphorus) were assessed from 24-h recalls. The group of swimmers had significantly lower BMI values than the control group. No systematic, significant between-group differences were found in nutrient intake or in bone mineralization variables. Calcium intake was below the recommended norm in all subjects but mean values of bone mineralization variables (BMC, BMD) steadily increased in both groups. The BMD z-scores proved negative throughout the three-year period of early adolescence in both groups of girls and that decrease was significant in swimmers. This could have been due to insufficient calcium intake as well as to inadequate calcium-to-phosphate and protein-to-calcium ratios and, when continued, might result in a decreased bone mass in adulthood.     

Tidal effects on the organic carbon mineralization rate under aerobic conditions in sediments of an intertidal estuary

Laboratory experiments and field measurements were conducted to examine the effect of tide on the organic carbon mineralization rate in sediments under aerobic conditions of an intertidal estuary. Core samples of surface sediments were collected from an intertidal estuary of the Kurose River, Hiroshima, Japan. To mimic low and high tide in the intertidal estuary, organic carbon mineralization rates in the samples were measured in the laboratory under both air-exposed and submerged conditions. Mineralization rates under air-exposed conditions were two to five times higher than those under submerged conditions. Field measurements of the rate of CO₂ emission from the sediment surface revealed a rapid increase in the rate as the sea level fell during ebb tide. The estimated amount of daily organic carbon mineralization assuming a constantly submerged condition was 30% less than that estimated when considering the semi-diurnal fluctuation in sea level. These results indicate that tide has a marked impact on the organic carbon mineralization rate in sediments under aerobic conditions on an intertidal estuary, and tidal effects need to be considered when the amount of mineralized organic carbon is estimated.     

氮磷添加对杉木林土壤碳氮矿化速率及酶动力学特征的影响

以江西杉木林红壤为研究对象,开展野外长期氮(N)、磷(P)添加控制试验,设置对照(CK)、N(50kg N hm~(-2)a~(-1))、P(50kg P hm~(-2)a~(-1))、NP(50kg N hm~(-2)a~(-1)+50kg P hm~(-2)a~(-1))处理,分析N、P添加对土壤碳矿化速率(C_(min))、氮矿化速率(N_(min))和相关的β-1,4-葡萄糖苷酶(βG)和β-1,4-N-乙酰葡糖氨糖苷酶(NAG)动力学参数的影响。结果表明:(1)N添加明显降低了C_(min)和N_(min),比CK分别减少了25%和18%;N添加减小了NAG的潜在最大酶活性(V_(max))、半饱和常数(K_m)、催化效率(V_(max)/K_m),但差异不显著(P0.05);N添加显著增加了βG的V_(max)、K_m,但对V_(max)/K_m有抑制作用。(2)P输入(P、NP)较CK使NAG的V_(max)、K_m减小26%—60%;NP同时添加明显提高βG和NAG的V_(max)/K_m(P0.05),但P输入(P、NP)对C_(min)和N_(min)影响不显著(P0.05)。(3)C_(min)与土壤溶解性有机碳正相关,N_(min)与pH显著正相关,与土壤NH_4~+-N、NO_3~--N显著负相关;βG和NAG的V_(max)/K_m均与NH_4~+-N、NO_3~--N负相关(P0.05),K_m均与NH_4~+-N、NO_3~--N正相关(P0.05)。βG的V_(max)与NH_4~+-N、NO_3~--N正相关(P0.05),NAG的V_(max)与有机碳、全氮、全磷、有效磷负相关(P0.05)。研究结果表明,在亚热带杉木人工林中,N添加降低土壤pH,增加土壤有效氮含量,抑制βG和NAG的V_(max)/K_m,对土壤C_(min)和N_(min)产生抑制作用;而NP添加增加土壤有效磷含量,增加土壤βG和NAG的V_(max)/K_m。     

Stathmin inhibits proliferation and differentiation of dental pulp stem cells via sonic hedgehog/Gli

The mineralization of dental pulp stem cells is an important factor in the tissue engineering of teeth, but the mechanism is not yet obvious. This study aimed to identify the effect of Stathmin on the proliferation and osteogenic/odontoblastic differentiation of human dental pulp stem cells (hDPSCs) and to explore whether the Shh signalling pathway was involved in this regulation. First, Stathmin was expressed in the cytoplasm and on the cell membranes of hDPSCs by cell immunofluorescence. Then, by constructing a lentiviral vector, the expression of Stathmin in hDPSCs was inhibited. Treatment with Stathmin shRNA (shRNA‐Stathmin group) inhibited the ability of hDPSCs to proliferate, as demonstrated by a CCK8 assay and flow cytometry analysis, and suppressed the osteogenic/odontoblastic differentiation ability, as demonstrated by alizarin red S staining and osteogenic/odontoblastic differentiation‐related gene (ALP, BSP, OCN, DSPP) activity, compared to that of hDPSCs from the control shRNA group. Molecular analyses showed that the Shh/GLI1 signalling pathway was inhibited when Stathmin was silenced, and purmorphamine, the Shh signalling pathway activator, was added to hDPSCs in the shRNA‐Stathmin group, real‐time PCR and Western blotting confirmed that expression of Shh and its downstream signalling molecules PTCH1, SMO and GLI1 increased significantly. After activating the Shh signalling pathway, the proliferation of hDPSCs increased markedly, as demonstrated by a CCK8 assay and flow cytometry analysis; osteogenic/odontoblastic differentiation‐related gene (ALP, BSP, OCN, DSPP) expression also increased significantly. Collectively, these findings firstly revealed that Stathmin‐Shh/GLI1 signalling pathway plays a positive role in hDPSC proliferation and osteogenic/odontoblastic differentiation.     

Isolation and Identification of Halophilic and Halotolerant Bacteria From Badab-e Surt Travertine Spring,Kiasar, Iran,and Investigation of Calcite Biomineralization Induction

Badab-e Surt spring is a travertine spring that has low to moderate levels of salt, so it is a good model for isolating moderately halophilic bacteria and investigating the relationship between microbe and environment. For isolating bacterial strains, water and sediment samples were collected from different springheads of the Badab-e Surt spring. Among the 171 bacterial isolates, 110 strains were halophiles. According to comparative partial 16S rRNA sequence analysis, the selected halophilic gram-positive and gram-negative strains were identified as members of the genera: Roseovarius, Labrenzia, Erythrobacter, Erythromicrobium, Massilia, Marinobacter, Halomonas, Shewanella, Pseudomonas, Flavobacterium, Bacillus, Brevibacterium, Staphylococcus, Microbacterium, Kocuria, and Streptomyces. To investigate mineralization, potential strains were screened by the culturing method, and then analyzed with a polarizing and scanning microscope. Five strains, Bss-11a, Bss-3, Bsw-1c1, Bsw-28d, and Bsw-39b, had potential for the mineralization of calcite that very closely resembled species Bacillus cohenii DSM 6307^T, Labrenzia aggregate IAM 12614^T, Bacillus safensis FO-036b^T, Marinobacter flavimaris SW-145^T, and Marinobater adhaerens HP15^T, respectively.     

Nitrogen mineralization and denitrification as influenced by crop residue particle size

Managing the crop residue particle size has the potential to affect N conservation in agricultural systems. We investigated the influence of barley (Hordeum vulgare) and pea (Pisum sativum) crop residue particle size on N mineralization and denitrification in two laboratory experiments. Experiment 1: ¹⁵N-labelled ground (3 mm) and cut (25 mm) barley residue, and microcrystalline cellulose+glucose were mixed into a sandy loam soil with additional inorganic N. Experiment 2: inorganic¹⁵ N and C₂H₂ were added to soils with barley and pea material after 3, 26, and 109 days for measuring gross N mineralization and denitrification.Net N immobilization over 60 days in Experiment 1 cumulated to 63 mg N kg^-1 soil (ground barley), 42 (cut barley), and 122 (cellulose+glucose). More N was seemingly net mineralized from ground barley (3.3 mg N kg^-1 soil) than from cut barley (2.7 mg N kg^-1 soil). Microbial biomass peaked at day 4 with the barley treatments and at day 14 with the cellulose+glucose whereafter the biomass leveled out at values 79 mg C kg^-1 (ground), 104 (cut), and 242 (cellulose+glucose) higher than for the control soil. Microbial growth yields were similar for the two barley treatments, ca. 60 mg C g^-1 substrate C added, which was lower than the 142 mg C g^-1 C added with cellulose+glucose. This suggests that the 75% (w/w) holocelluloses and sugars contained with the barley material remained physically protected despite grinding. In Experiment 2 gross mineralization on day 3 was 4.8 mg N kg^-1 d^-1 with ground pea, twice as much as for all other treatments. On day 26 the treatment with ground barley had the greatest gross N mineralization. In static cores ground barley denitrified 11-fold more than did cut barley, whereas denitrification was similar for the two pea treatments. In suspensions denitrification was similar for the two treatments both with barley and pea residue.We conclude that the higher microbial activity associated with the initial decomposition of ground plant material is due to a more intimate plant residue-soil contact. On the long term, grinding the plant residues has no significant effect on N dynamics.     

Nitrogen availability and uptake by grassland in mesocosms at two water levels and two water qualities

We studied the effect of water table (-5 or -30 cm) and water type (rain- or groundwater) on the above- and below-ground phytomass production, species composition and nitrogen uptake of grassland.Nitrogen mineralization, nitrification, methane production, redox potential and pH at different depths in the profile were measured and used to monitor gradual changes in variables influencing phytomass production.The rise in the water level lowered the nitrogen uptake in the above-ground phytomass from 14.1 to 11.4 g N per m², but the DM production did not decrease and varied from 566 to 690 g per m². The total root mass increased from 82 to 363 g DM per m², with the proportion in the 5 to 10 cm layer increasing the most from 13 to 24%.The high water level lowered the potential N mineralization in the upper 5 cm of the soil from 16.1 to 4.3 g N per m² and in the deeper 5 to 30 cm layer from 12.6 to 9.4 g N per m² respectively, so the importance of the deeper layer as a source of N increased. The total amount of mineral N that accumulated in the 40 cm deep soil cores decreased from 31.3 to 15.5 g N per m². The above-ground vegetation took up 71 to 76% of this amount in the high water level treatment and only 37 to 57% under drier conditions.Redox potential and methane production indicated anaerobic conditions below 5 cm in both level treatments and in the top 5 cm of the high water level treatment. But some nitrification was measured there also, thus aerobic and anaerobic conditions occurred together. The low N mineralization was attributed to low soil respiration.Raising the water level brought about an increase in the above ground biomass of Glyceria fluitans and an increase in root mass, especially deeper in the soil. Both are responsible for the relatively greater fraction of nitrogen that was taken up from the soil, although less N was available. The nitrification indicates that oxygen is transported by the root system to soil microsites and partly compensates for the anaerobic conditions caused by water saturation.The calcareous groundwater raised the pH in the upper soil layer from 5.3 to 5.8 but no effect on N mineralization was measured.