丹参素注射液对急性心肌梗死大鼠的心室重构、心室功能及肢体导联与胸导联心电图参数的影响

摘要 目的：探讨丹参素注射液对急性心肌梗死大鼠的心室重构、心室功能及肢体导联与胸导联心电图参数的影响。方法：选择SD大鼠40只,将其鼠随机模型组、假手术组、硝酸甘油组、丹参注射液组。假手术组大鼠给予只在冠状动脉处穿针,不进行结扎,其余步骤同其余3组,其余3组均进行动物模型构建。假手术组、模型组大鼠均腹腔注射氯化钠注射液,硝酸甘油组腹腔注射硝酸甘油,丹参注射液组腹腔注射丹参注射液。对比4组大鼠的肢体导联与胸导联心电图参数,对比4组大鼠的血液流变学指标、左心室功能及左心室重构。结果：模型组的Ⅰ、Ⅱ、Ⅲ、aVL、aVF、V1、V2、V5、血浆粘度、纤维蛋白原、红细胞聚集指数、舒张末期室间隔厚度、左室舒张末期内径、左室收缩末期内径、左室舒张末期容积、左室收缩末期容积明显较假手术组、硝酸甘油组、丹参注射液组高,硝酸甘油、丹参注射液组以上指标明显较假手术组高,模型组的的左室舒张末期厚度、左室射血分数、左室短轴缩短率明显较假手术组、硝酸甘油组、丹参注射液组低,硝酸甘油、丹参注射液组的左室舒张末期厚度、左室射血分数、左室短轴缩短率明显较假手术组低。模型组的左心室重量指数、左心室截面直径明显较假手术组、硝酸甘油组、丹参注射液组高,硝酸甘油、丹参注射液组的左心室重量指数、左心室截面直径、梗死面积明显较假手术组高（P<0.05）,硝酸甘油组与丹参注射液组以上指标对比无差异（P>0.05）。结论：丹参素注射液可改善急性心肌梗死大鼠的心室重构、左心室功能及肢体导联与胸导联心电图参数,可能与其可降低大鼠的血液流变学指标水平有关。     

血清PGRN、SFRP1、CCL26与支气管哮喘急性发作期患者肺功能和气道炎症的相关性研究

摘要 目的：探讨支气管哮喘（BA）急性发作期患者血清颗粒蛋白前体（PGRN）、分泌型卷曲相关蛋白1（SFRP1）、C-C基序趋化因子配体26（CCL26）与肺功能和气道炎症的相关性。方法：选取2021年1月～2022年6月我院收治的118例BA急性发作期患者作为急性发作期组,根据病情分级将BA急性发作期患者分为轻度亚组55例、中度亚组43例、重度亚组20例,另选取同期77例BA临床控制期患者（临床控制期组）和60例体检健康志愿者（对照组）分别作为对照。采用Pearson相关性分析BA急性发作期患者血清PGRN、SFRP1、CCL26水平与肺功能和气道炎症指标的相关性。结果：对照组、临床控制期组、急性发作期组血清PGRN水平和第1秒用力呼气容积占预计值百分比（FEV₁%pred）、峰值呼气流速（PEF）依次降低,SFRP1、CCL26水平和呼出气一氧化氮（FeNO）、外周血嗜酸性粒细胞（EOS）计数依次升高（P＜0.05）。轻度亚组、中度亚组、重度亚组血清PGRN水平和FEV₁%pred、PEF依次降低,SFRP1、CCL26水平和FeNO、外周血EOS计数依次升高（P＜0.05）。Pearson相关性分析显示,BA急性发作期患者血清PGRN水平与FEV₁%pred、PEF呈正相关,与FeNO、外周血EOS计数呈负相关（P＜0.05）,SFRP1、CCL26与FEV₁%pred、PEF呈负相关,与FeNO、外周血EOS计数呈正相关（P＜0.05）。结论：BA急性发作期患者血清PGRN水平降低,SFRP1、CCL26水平升高,与病情严重程度、肺功能和气道炎症有关,可能成为BA急性发作期患者新的治疗靶点。     

介入栓塞术在急诊难治性医源性肾出血中的临床应用价值

摘要 目的：探讨介入栓塞术在急诊难治性医源性肾出血中的临床应用价值。方法：收集2012年6月至2021年6月南京医院大学第一附属医院收治的72例急诊难治性医源性肾出血的患者。所有患者在保守治疗无效的情况下,行介入下肾动脉血管造影,根据造影表现确定出血责任动脉,并行栓塞治疗,术后观察临床止血的有效性及安全性。结果：72例患者,介入血管造影呈阳性结果64例,包括血管出现单纯造影剂外溢12例,单纯假性动脉瘤19例,单纯动静脉瘘8例,9例患者合并两种造影表现,以及16例患者呈现动脉出血的一些间接征象。阳性出血患者介入栓塞技术成功率及临床止血率为100%。72例患者介入术后3 d血白细胞、血中性粒细胞比率、血红蛋白、血细胞比容及血小板较术前明显升高（均P＜0.05）,血肌酐及尿素氮较介入术前轻度升高（均P＞0.05）;其中30例患者介入术后7 d再次检测血肌酐及尿素氮,较介入术前基本恢复正常（均P＞0.05）。住院期间所有患者未出现肾衰等严重的术后并发症。结论：介入栓塞术治疗急诊难治性医源性肾出血患者,具有安全、高效、并发症少等优点,临床上值得推广应用。     

Effect of modification of storage atmosphere on phospholipids and ultrastructure of cauliflower mitochondria

Differences in mitochondrial membrane composition and ultrastructure were studied after storage of cauliflower ( Brassica oleracea , L., Botrytis group) for 5 days at 25°C in air or under controlled atmospheres: 3% O₂, 21% O₂+ 15% CO₂ or 3% O₂+ 15% CO₂. In air, postharvest senescence involved a 20% decrease in mitochondrial phospholipid content. A large reduction in the relative abundance of phosphati-dylcholine (PC) and in the degree of unsaturation of PC and phosphatidyl ethanolamine (PE) was observed. However, the degree of unsaturation increased in cardiolipin (CL). Storage under 3% O₂ did not prevent phospholipid breakdown. Low O₂ prevented the relative decrease in PC observed during storage in air and the loss of linoleic acid from PC, but not from PE. This relative protection offered by the low O₂ atmosphere was lost under 3% O₂+ 15% CO₂. The high CO₂ atmospheres caused twice as much loss in phospholipids as that observed during storage in air. Extensive loss of mitochondrial protein, a marked decrease in phospholipid to protein ratio, and electron micrograph observations suggest structural alterations in the presence of high CO₂.     

Effect of nitrogen application on growth and photosynthetic nitrogen use efficiency in two ecotypes of wild strawberry, Fragaria chiloensis

The relationships between increasing nitrogen fertilization and growth, maximum CO₂ assimilation and the initial slope of the CO₂ response curve were studied in 2 ecotypes of wild strawberry, Fragaria chiloensis (L.) Duchn. Nitrogen accumulation of CA11, an ecotype from a low-nutrient dune site, was greater at all nitrogen concentrations than that of RCP37, an ecotype from a higher-nutrient strand site. Maximum CO₂ assimilation, total Rubisco activity, dry weight, and initiation of leaves and crowns were higher in CAI1 than RCP37 as nitrogen treatment was increased from 0 to 200 mg ^l-1, whereas these parameters were lower in CAl1 when fertilized at 300 mg T¹, but not in RCP37. The mean leaf area of CA11 was greater than RCP37 when grown with no supplemental nitrogen, but mean leaf area of the 2 lines was similar under nitrogen fertilization. Maximum CO₂ assimilation and carboxylation efficiency increased with increasing leaf nitrogen in both clones. At equivalent concentrations of leaf nitrogen, RCP37 had higher CO₂ assimilation and carboxylation efficiency than CA11 and the difference between the 2 clones increased as ieaf nitrogen increased. Thus, RCP37 had a higher photosynthetic nitrogen use efficiency than CA11. However, at a given applied nitrogen level, CA11 allocated more nitrogen to a unit of leaf area so that photosynthetic rates were higher than RCP37, except at the highest application of 300 mg ^l-1. The high nitrogen accumulation capacity and resource allocation to fruiting structures (crowns) in CA11 leads us to suggest that this clone may possess genes that could increase fruit yield in cultivated strawberry.     

Effects of elevated atmospheric CO2 on net ecosystem CO2 exchange of a scrub–oak ecosystem

We report the results of a 2‐year study of effects of the elevated (current ambient plus 350 μmol CO₂ mol^?1) atmospheric CO₂ concentration (C_a) on net ecosystem CO₂ exchange (NEE) of a scrub–oak ecosystem. The measurements were made in open‐top chambers (OTCs) modified to function as open gas‐exchange systems. The OTCs enclosed samples of the ecosystem (ca. 10 m² surface area) that had regenerated after a fire, 5 years before, in either current ambient or elevated C_a. Throughout the study, elevated C_a increased maximum NEE (NEE_max) and the apparent quantum yield of the NEE (φ_NEE) during the photoperiod. The magnitude of the stimulation of NEE_max, expressed per unit ground area, was seasonal, rising from 50% in the winter to 180% in the summer. The key to this stimulation was effects of elevated C_a, and their interaction with the seasonal changes in the environment, on ecosystem leaf area index, photosynthesis and respiration. The separation of these factors was difficult. When expressed per unit leaf area the stimulation of the NEE_max ranged from 7% to 60%, with the increase being dependent on increasing soil water content (W_soil). At night, the CO₂ effluxes from the ecosystem (NEE_night) were on an average 39% higher in elevated C_a. However, the increase varied between 6% and 64%, and had no clear seasonality. The partitioning of NEE_night into its belowground (R_below) and aboveground (R_above) components was carried out in the winter only. A 35% and 27% stimulation of NEE_night in December 1999 and 2000, respectively, was largely due to a 26% and 28% stimulation of R_below in the respective periods, because R_below constituted ca. 87% of NEE_night. The 37% and 42% stimulation of R_above in December 1999 and 2000, respectively, was less than the 65% and 80% stimulation of the aboveground biomass by elevated C_a at these times. An increase in the relative amount of the aboveground biomass in woody tissue, combined with a decrease in the specific rate of stem respiration of the dominant species Quercus myrtifolia in elevated C_a, was responsible for this effect. Throughout this study, elevated C_a had a greater effect on carbon uptake than on carbon loss, in terms of both the absolute flux and relative stimulation. Consequently, for this scrub–oak ecosystem carbon sequestration was greater in the elevated C_a during this 2‐year study period.     

Soil 13C–15N dynamics in an N2-fixing clover system under long-term exposure to elevated atmospheric CO2

Reduced soil N availability under elevated CO₂ may limit the plant's capacity to increase photosynthesis and thus the potential for increased soil C input. Plant productivity and soil C input should be less constrained by available soil N in an N₂‐fixing system. We studied the effects of Trifolium repens (an N₂‐fixing legume) and Lolium perenne on soil N and C sequestration in response to 9 years of elevated CO₂ under FACE conditions. ¹⁵N‐labeled fertilizer was applied at a rate of 140 and 560 kg N ha^?1 yr^?1 and the CO₂ concentration was increased to 60 Pa pCO₂ using ¹³C‐depleted CO₂. The total soil C content was unaffected by elevated CO₂, species and rate of ¹⁵N fertilization. However, under elevated CO₂, the total amount of newly sequestered soil C was significantly higher under T. repens than under L. perenne. The fraction of fertilizer‐N (f_N) of the total soil N pool was significantly lower under T. repens than under L. perenne. The rate of N fertilization, but not elevated CO₂, had a significant effect on f_N values of the total soil N pool. The fractions of newly sequestered C (f_C) differed strongly among intra‐aggregate soil organic matter fractions, but were unaffected by plant species and the rate of N fertilization. Under elevated CO₂, the ratio of fertilizer‐N per unit of new C decreased under T. repens compared with L. perenne. The L. perenne system sequestered more ¹⁵N fertilizer than T. repens: 179 vs. 101 kg N ha^?1 for the low rate of N fertilization and 393 vs. 319 kg N ha^?1 for the high N‐fertilization rate. As the loss of fertilizer‐¹⁵N contributed to the ¹⁵N‐isotope dilution under T. repens, the input of fixed N into the soil could not be estimated. Although N₂ fixation was an important source of N in the T. repens system, there was no significant increase in total soil C compared with a non‐N₂‐fixing L. perenne system. This suggests that N₂ fixation and the availability of N are not the main factors controlling soil C sequestration in a T. repens system.     

Soil-surface carbon dioxide efflux and microbial biomass in relation to tree density 13 years after a stand replacing fire in a lodgepole pine ecosystem

The effects of fire on soil‐surface carbon dioxide (CO₂) efflux, F_S, and microbial biomass carbon, C_mic, were studied in a wildland setting by examining 13‐year‐old postfire stands of lodgepole pine differing in tree density (< 500 to > 500 000 trees ha^?1) in Yellowstone National Park (YNP). In addition, young stands were compared to mature lodgepole pine stands (～110‐year‐old) in order to estimate ecosystem recovery 13 years after a stand replacing fire. Growing season F_S increased with tree density in young stands (1.0 µmol CO₂ m^?2 s^?1 in low‐density stands, 1.8 µmol CO₂ m^?2 s^?1 in moderate‐density stands and 2.1 µmol CO₂ m^?2 s^?1 in high‐density stands) and with stand age (2.7 µmol CO₂ m^?2 s^?1 in mature stands). Microbial biomass carbon in young stands did not differ with tree density and ranged from 0.2 to 0.5 mg C g^?1 dry soil over the growing season; C_mic was significantly greater in mature stands (0.5–0.8 mg C g^?1 dry soil). Soil‐surface CO₂ efflux in young stands was correlated with biotic variables (above‐ground, below‐ground and microbial biomass), but not with abiotic variables (litter and mineral soil C and N content, bulk density and soil texture). Microbial biomass carbon was correlated with below‐ground plant biomass and not with soil carbon and nitrogen, indicating that plant activity controls not only root respiration, but C_mic pools and overall F_S rates as well. These findings support recent studies that have demonstrated the prevailing importance of plants in controlling rates of F_S and suggest that decomposition of older, recalcitrant soil C pools in this ecosystem is relatively unimportant 13 years after a stand replacing fire. Our results also indicate that realistic predictions and modeling of terrestrial C cycling must account for the variability in tree density and stand age that exists across the landscape as a result of natural disturbances.     

应用FIA型微生物传感器测定谷氨酸含量的研究

目前应用酶或微生物细胞作为分子识别元件构建生物传感器测定谷氨酸含量的研究引起了广泛的兴趣,并陆续有实例报道。在这些报道中人们依据不同的酶催反应选择相应的离子选择性电极,如CO₂电极、NH₄⁺电极等,而测量对象有直接的测定谷氨酸,也有测定谷氨酸单钠的间接测定法。本文选用了可固定大量细胞的固定化细胞柱与流动注入法相结合的测量方法,并根据细胞柱的动力学模型分析动态响应曲线,计算测量结果,提高了测量精度,扩大了测量范围。     

Stomatal and nonstomatal limitations of photosynthesis in relation to the drought and shade tolerance of tree species in open and understory environments

 Light saturated photosynthesis (A) in field saplings of shade tolerant, intermediate, and intolerant tree species was analyzed for stomatal and nonstomatal limitations to test differences between species and sun and shade phenotypes during drought. Throughout the study, photosynthesis was highest and mesophyll limitations of A (L_m) lowest in the intolerant species in both open and understory habitats. The shade tolerant species exhibited the only drought-related decreased A and increased L_m in the open, and the greatest drought-related decreased A and increased L_m in the understory. Few species exhibited significant habitat or drought-related differences in stomatal conductance to CO₂ (g_c), but even slight decreases in g_c during drought were associated with large increases in stomatal limitations to A (L_g). Combined changes in L_m and L_g resulted in increased relative stomatal limitation to A (l _g) in several species during drought. Nevertheless, the overall lack of stomatal closure allowed for nonstomatal limitations to play a major role in reduced A during drought. Higher leaf N was associated with shallower slope of the l _g versus g_c relationship, an indication of greater A capacity. Photosynthetic capacity tended to be greater in the intolerant species than the tolerant species, and it tended to decrease during drought primarily in the shade tolerant species in the understory. Findings in the literature suggest that carbon reduction reactions may be more susceptible to drought than photosynthetic light reactions. If so, reduced carbon reduction capacity of shade tolerant species or shade phenotypes may predispose them to drought conditions, which suggests a mechanism behind the well-recognized tradeoff between drought tolerance and shade tolerance of temperate tree species. Received: 20 October 1995 / Accepted: 20 February 1996