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1.
A 71-year-old woman came to the hospital with a 24-hour-old occlusion of the left limb of an aortoiliac knitted Dacron graft and was treated with an intra-arterial infusion of urokinase, 40,000 U/hr. Although the graft limb was successfully recanalized in 16 hours, the patient suffered a massive retroperitoneal hemorrhage through the wall of the graft. Clinicians must be aware of this potentially serious complication of thrombolytic therapy in patients with thrombosed, knitted Dacron grafts.  相似文献   
2.
In situ saphenous vein grafts are being used with increasing frequency for bypass procedures involving the femoral and popliteal arteries. Complications of these procedures include anastomotic stenoses and persistent arteriovenous fistulae that may result in failure of the graft. Balloon angioplasty and embolotherapy with detachable balloons were employed successfully in three or four recent cases of patients with complications from in situ grafts. Tailored angiography is essential for evaluating in situ grafts, and interventional techniques are extremely useful for managing complications.  相似文献   
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As an alternative to performing interventional radiology on inpatients under the care of internists and surgeons, the authors have established a cardiovascular radiology admitting service for well-screened, elective patients. The patients are admitted under the care of a cardiovascular radiology fellow and a staff physician. From April 1982 to December 1983, 133 patients were admitted to the service. Patients are cared for in a surgical ward or in an intermediate unit, as determined by the clinical situation. Advantages of this approach include a broader patient referral base, improved rapport with clinical colleagues and patients, improved follow-up data, and rapid evaluation and treatment, resulting in short hospital stays. The major disadvantages involve the commitment of time and staff necessary to provide quality care. The concept of the interventional radiologist in the role of admitting physician has important implications in terms of negotiations for additional financial compensation, commensurate with the skill and time required for performing these procedures and caring for the patient.  相似文献   
7.
Kinnison  ML; Powe  NR; Steinberg  EP 《Radiology》1989,170(2):381-389
The authors reviewed 100 randomized controlled trials (RCTs) conducted in humans to compare safety or efficacy of new low-osmolality contrast media (LOM) with that of high-osmolality contrast media (HOM). Findings of the 43 RCTs judged to be of the highest quality suggest that the efficacy of LOM in imaging is equal or superior to that of HOM for all routes of administration. Heat sensation occurred less often with LOM for all routes and pain occurred less often with LOM for intraarterial routes. No differences were seen in nephrotoxicity or in frequency of nausea, vomiting, urticaria, bronchospasm, laboratory test abnormalities, or neurologic events. Greater cardiovascular changes were seen with HOM, including increased or decreased heart rate, increased left ventricular end-diastolic pressure, decreased systolic pressure, and QT prolongation, depending on route of administration. To demonstrate whether a reduction in clinically significant adverse outcomes truly occurs with LOM, trials will need to enlist larger numbers of patients and employ appropriate outcome measures. Future trials should stratify patients according to their risk of adverse reactions to provide better information about benefits of LOM in low- versus high-risk patients.  相似文献   
8.
BACKGROUND: Most suicides (60%) and homicides (67%) are committed with firearms. Additionally, 90% of homicide offenders and 80% of individuals reporting suicide behaviors meet diagnostic criteria for mental illness. Medical society guidelines support the counseling of patients regarding firearms. This study assessed psychiatrists' anticipatory guidance on firearms and their perceived roles on this topic. METHOD: A four-wave mail survey of adult psychiatrists in Ohio was conducted and analyzed. The outcome measures were the portion of psychiatrists involved in anticipatory guidance on firearm safety issues and their self-efficacy and perceived barriers regarding firearm counseling. RESULTS: Two hundred and five psychiatrists of a possible 340 (60%) responded. Almost half (45%) had never thought seriously about discussing firearm safety issues with patients. They perceived firearm safety issues to be much greater (32%) or slightly greater (37%) for mental health patients than for the general population. Psychiatrists with high efficacy expectations were twice as likely (56.5% vs 28.0%) as those with low efficacy expectations to provide firearm anticipatory guidance. Those who counseled their patients were 15 times more likely to have high outcome expectations compared to those who did not counsel their patients (93.7% vs 6.3%, respectively). CONCLUSIONS: When psychiatrists are provided with firearm information, they were significantly more likely to be involved in anticipatory guidance regarding firearms. This implies that professional societies and journals should attempt to increase the information they provide to their members regarding this topic. Psychiatrists may be in a unique position to help reduce firearm morbidity and mortality for mentally ill patients.  相似文献   
9.
Very short-lived brominated substances (VSLBr) are an important source of stratospheric bromine, an effective ozone destruction catalyst. However, the accurate estimation of the organic and inorganic partitioning of bromine and the input to the stratosphere remains uncertain. Here, we report near-tropopause measurements of organic brominated substances found over the tropical Pacific during the NASA Airborne Tropical Tropopause Experiment campaigns. We combine aircraft observations and a chemistry−climate model to quantify the total bromine loading injected to the stratosphere. Surprisingly, despite differences in vertical transport between the Eastern and Western Pacific, VSLBr (organic + inorganic) contribute approximately similar amounts of bromine [∼6 (4−9) parts per thousand] to the stratospheric input at the tropical tropopause. These levels of bromine cause substantial ozone depletion in the lower stratosphere, and any increases in future abundances (e.g., as a result of aquaculture) will lead to larger depletions.Until the end of the last century, it was believed that only long-lived species, like bromomethane (CH3Br) and halons, contributed to the global burden of stratospheric bromine. However, disagreement between the observed amount of reactive stratospheric bromine and the sources of long-lived trace gases suggested the existence of an additional contributor: Very short-lived brominated substances (VSLorg) [VSLorg = bromoform (3CHBr3) + dibromomethane (2CH2Br2) + minorVSLBr, where minorVSLBr = bromochloromethane (CH2BrCl) + dibromochloromethane (2CHBr2Cl) + bromodichloromethane (CHBrCl2)] that originate mainly from ocean biogenic sources (1, 2).Several studies have described the processes involved in the transformation of biogenic bromocarbons to inorganic bromine, and their transport through the tropical tropopause layer (TTL) (15). These studies have led to significant progress in modeling the VSLorg contribution to the formation of stratospheric inorganic bromine (Bry) (3, 4, 611). However, the scarcity of observations to constrain the emissions, the impact of deep convection, and the effect of dehydration processes limit the prediction of short-lived source gases that reach the stratosphere (3). On the other hand, atmospheric observations of VSLorg have been provided by ground measurements and cruise, balloon, and airborne campaigns (1214), but the different instruments used between campaigns, and the low spatial and temporal coverage of each study, contribute to the uncertainties in the estimations of total bromine and its partitioning (15). In an attempt to reduce these limitations, we present unique measurements of organic bromine substances carried out with the same instrument, the Global Hawk Whole Air Sampler (GWAS), deployed during the NASA Airborne Tropical Tropopause Experiment (ATTREX), which covered the tropical Pacific region during 2013 and 2014 (see SI Text for details of the campaign).Because coastal areas of tropical waters (like the Maritime Continent) are an important source for VSLorg (1618) and highly convective zones can transport air masses from the troposphere into the stratosphere through the TTL (19), we focus this study on observations taken over the Western Pacific (120°E−165°E) and the Eastern Pacific (187°E−268°E) (Fig. S1). We compared these regions in terms of VSLorg mixing ratios at the tropopause level (∼17 km; Fig. S2), which defines the chemical composition of air that enters the stratosphere.Open in a separate windowFig. S1.GWAS sample locations during ATTREX campaign. Dotted lines define the Western (120°E–165°E) and Eastern Pacific (187°E–268°E) limits for this study.Open in a separate windowFig. S2.Sample density of measurements of organic bromine species (A) during ATTREX-2014 (Western Pacific) and (B) during ATTREX-2013 (Eastern Pacific).Whole air samples were collected during two deployments of the ATTREX campaigns, on board the unmanned aerial vehicle Global Hawk. Measurements of VSLorg were carried out in the field using a combination of gas chromatography with mass selective, flame ionization, and electron capture detectors (Materials and Methods). Fig. 1 A and B displays the observations of CHBr3, CH2Br2, and minorVSLBr, as well as the total organic bromine mixing ratio, in the upper troposphere/lower stratosphere (UTLS) of the Western and Eastern Pacific. GWAS observations indicate that the total amount of VSLorg that enters the stratosphere over the Western and Eastern Pacific is approximately similar, 3.27 ± 0.47 parts per thousand (ppt) and 2.96 ± 0.42 ppt, respectively. These observations are compared with the state-of-the-art Community Atmosphere Model (CAM-Chem) simulations (4, 20) (see Materials and Methods). The results show good agreement with the measurements, and simulate the injection of VSLorg to the stratosphere of 3.84 ± 0.64 ppt and 3.18 ± 1.49 ppt organic Br for the Western and Eastern Pacific, respectively (Fig. 1 A and B).Open in a separate windowFig. 1.GWAS measurements and CAM-Chem simulations ±1 SD. Filled symbols are the 1 km average bins from GWAS measurements. Lines are the CAM-Chem simulation. Values from the arrows represent the mean mixing ratio (ppt) of VSLorg and Bry at the tropopause level (∼17 km) derived from CAM-Chem simulations. (A and B) Organic brominated species multiplied by their atomicity for (A) Western Pacific and (B) Eastern Pacific. (C and D) CAM-Chem estimations of inorganic bromine (Bry) from measured brominated VSLS with shaded ±1 SD for (C) Western Pacific and (D) Eastern Pacific.Although negligible differences of the organic fraction of VSLBr were observed between the Western and Eastern Pacific, we quantified the inorganic fraction coming from the degradation of VSLorg. Estimations of inorganic bromine (Bry = Br + BrO + HOBr + BrONO2 + HBr + BrCl + 2Br2 + BrNO2 + IBr), with a focus at ∼17 km, were calculated with the CAM-Chem model using assimilated meteorological fields for each Global Hawk flight. According to these simulations, the amount of Bry over the Eastern Pacific is 3.02 ± 1.90 ppt, whereas, in the Western Pacific, the mixing ratio of Bry is 1.97 ± 0.21 ppt (Fig. 1 C and D). Bry/VSLorg ratios show that at ∼17 km, the abundance of Bry over the Western Pacific is almost half the amount of VSLorg, in contrast to the Eastern Pacific, where the abundance of Bry is similar to the value of VSLorg (
Values at 17 kmWestern PacificEastern Pacific
From CAM-Chem
 VSLorg, ppt3.84 ± 0.643.18 ± 1.49
 Bry, ppt1.97 ± 0.213.02 ± 1.90
 Bry/VSLorg0.51 ± 0.040.95 ± 0.32
 VSLBr (Bry + VSLorg),* ppt5.81 ± 0.676.20 ± 2.41
From GWAS
 VSLorg, ppt3.27 ± 0.472.96 ± 0.42
 VSLBr (Bry + VSLorg), ppt5.24 ± 0.515.98 ± 1.95
Open in a separate window*VSLBr from CAM-Chem. Both VSLorg and Bry are estimates from CAM-Chem model.VSLBr from GWAS. VSLorg are the measurements from GWAS, and Bry are estimates from CAM-Chem model.We evaluated these different Bry/VSLorg ratios with 12-d back-trajectory analyses using the Numerical Atmospheric dispersion Modeling Environment (NAME) (21) (see Materials and Methods). These analyses indicate that a variety of source regions influenced our samples in the TTL during the ATTREX flights (see SI Text for details). However, the majority of air transported to the tropopause region (∼17 km) of the Eastern and Western Pacific last encountered the boundary layer in the area between 90°E and −140°E (Fig. S3). Fig. 2 A and B shows two representative cases of the locations where the back-trajectories first crossed the 1-km-altitude surface for samples collected over the Western and Eastern Pacific, respectively. This similarity on the source location of the air mass could explain the similar amount of VSLorg observed over both the Western and Eastern Pacific. The NAME analysis indicates that the mean time for the boundary layer (<1 km) air to reach the air sampled at 17 km was 9.8 d in the West Pacific samples and 11.1 d in the East Pacific. This difference in mean times, along with the difference between East and West Pacific in the fraction of trajectories that reach 1 km, is consistent with the observed differences in the mixing ratios of the shorter-lived gases such as methyl iodide, bromoform, and propane (Fig. 2C and Fig. S4D). This is supported by 30-d back-trajectories calculated by NAME, which show that the influence of convective events between days 12 and 30 was small. The same analyses show that differences of Bry could be due to transport dynamics, mixing processes, and age of air masses targeted during the field campaigns. Flights over the Western Pacific tracked fresh air from the air masses detrained into the TTL by Tropical Storm Faxai and air from the South Pacific Convection Zone. Thus, most of the air masses that reached ∼17 km during these two events moved from the boundary layer to the upper troposphere (UT) rather than following the horizontal pattern seen on most of the air masses tracked over the Eastern Pacific (Fig. 2 C and D). We suggest that these “fresh” air masses, quickly transported to the UT, limit the chemistry that leads to the formation of Bry, and reduce their abundance over the Western Pacific. From another point of view, the higher stratospheric injection of Br over the Eastern Pacific could be also related to transport time and distance. For example, as the air masses travel from West to East, heterogeneous recycling reactions could put more Br back into the troposphere than washout is removing. Previous studies have pointed out that rapid uplift of air masses, due to convection events, as well as the colder temperatures within the TTL, can considerably enhance the efficiency of heterogeneous reactions relative to complete washout or ice removal (3, 4, 22, 23). However, the impact of heterogeneous reactions depends on several factors, including the microphysical environment and the partitioning of the inorganic bromine species. Hence, further analysis of the Bry chemical speciation over the Eastern and Western Pacific could provide insight into these fundamental processes.Open in a separate windowFig. 2.NAME 12-d back-trajectories for samples collected over the Western Pacific (A and C) on 4 March 2014 (at 16.58 km, 18.341°N, 147.494°E), and over the Eastern Pacific (B and D) on 22 February 2013 (at 16.54 km, 12.007 °N, 107.82°W). (A and B) Location at which trajectories first crossed 1 km, with the color indicating the time taken to reach this altitude. Black line indicates the ATTREX flight path. Light blue mark represents the location of the GWAS sample where the trajectories start. (C and D) Probability distribution of trajectory altitude as a function of time traveled backward. The median trajectory altitude is marked with a solid line, 25th and 75th percentiles are marked with dotted lines, and 10th and 90th percentiles are marked with dot−dash lines.Open in a separate windowFig. S3.The dots mark the location of all particles released for samples collected between 16.5 km and 17.5 km (average ∼17 km) that passed through the 1-km surface. The color code indicates the time taken to reach this altitude. (A) Eastern Pacific and (B) Western Pacific.

Table S1.

Mixing ratio of other trace gases measured by GWAS during ATTREX campaign, and estimates of decrease from Western Pacific source location
Mixing ratio, pptPercent difference of average mixing ratio between Western and Eastern PacificMean time of air fraction below 1 km, daysTropics lifetime,* daysExponential decayFraction of decrease
Western PacificEastern PacificWestern PacificEastern PacificWestern PacificEastern Pacific
CHBr31.15 ± 0.430.93 ± 0.38199.811.1170.5620.5210.07
Propane22.91 ± 13.4918.53 ± 6.24199.811.113.50.4840.4390.09
CH3I0.07 ± 0.060.03 ± 0.01579.811.13.50.0610.0420.31
Open in a separate window*The 2014 WMO O3 assessment: 10 km tropics (25°S–25°N) annually averaged local lifetime (days) from total loss process.Mixing ratios multiplied by Br atomicity.Open in a separate windowFig. S4.NAME 12-d back-trajectories over the Western Pacific (A and C) on 4 March 2014 (origin at 14.43 km, 17.65°N, 147.43°E), and over the Eastern Pacific (B and D) on 22 February 2013 (origin at 14.34 km, 6.77°N, 101.69°W). (A and B) Location at which trajectories first crossed 1 km, with the color indicating the time taken to reach this altitude. Black line indicates the ATTREX flight path. Light blue marks represent the location of the GWAS sample where the trajectories start. (C and D) Probability distribution of trajectory altitude as a function of time traveled backward. The median trajectory altitude is marked with a solid line, 25th and 75th percentile are marked with dotted lines, and 10th and 90th percentile are marked with dot−dash lines.Based on the CAM-Chem simulation results, the overall contribution of VSL substances (VSLorg + Bry) to total stratospheric bromine, quantified at ∼17 km, show 5.81 (5.14–6.48) ppt over the Western Pacific and 6.20 (3.79–8.61) ppt over the Eastern Pacific (24). Note that this estimate based on model results is slightly higher and has a slightly narrower range than the 2014 WMO O3 assessment. However, using the same methodology as the 2014 WMO O3 assessment, GWAS measurements show that the contribution of VSL substances to total stratospheric bromine would be slightly lower [i.e., 5.24 (4.73–5.75) ppt over the Western Pacific and 5.98 (4.03–7.93) ppt over the Eastern Pacific (Fig. S5 A and B). Halon 1301 was not measured during ATTREX, and its contribution to the Br budget was estimated from measurements at surface sites (25). Remarkably, the results show similar profiles in the UTLS, and relatively little variation, between the Eastern and Western Pacific. In addition, CAM-Chem model simulations clearly capture the distribution and variability of these three major groups. The total organic bromine budgets at the tropopause (17 km, θ ≈ 370 K) resulted in 18.02 ± 0.66 ppt and 17.68 ± 0.49 ppt in the Western and Eastern Pacific, respectively (26, 27) and to the total organic bromine of 17.5 ± 0.6 ppt found over the Eastern Pacific during NASA-Costa Rica-Aura Validation Experiment (NASA-CRAVE) 2006 (https://espoarchive.nasa.gov/archive/browse/cr_ave). The similarity between campaigns over this extended time period reflects the changing abundances of the long-lived species (bromomethane and halons) and the variable amounts of short-lived bromine compounds found during the few campaigns that have collected data in the tropical TTL (25, 28, 29). During the time period from 1996 until 2014, methyl bromide has been declining globally (28). The global average of CH3Br has been reduced by ∼3.5 parts per trillion volume (pptv) during this time. At the same time, the total amount of halons has seen an increasing trend that reached a broad maximum during 2004–2008, and has slowly declined since then. For the missions shown in STRAT 1996*CRAVE 2006ATTREX 2013–2014Campaign locationCentral Pacific, ppt (%)Eastern Pacific, ppt (%)Western Pacific, ppt (%)Eastern Pacific, ppt (%)Halons6.63 ± 0.22 (38)8.26 ± 0.09 (47)7.59 ± 0.19 (42)7.92 ± 0.11 (45)CH3Br9.45 ± 0.39 (54)7.83 ± 0.16 (45)7.16 ± 0.41 (40)6.80 ± 0.23 (38)VSLorg1.30 ± 0.40 (7)1.42 ± 0.52 (8)3.27 ± 0.49 (18)2.96 ± 0.42 (17)Total organic bromine budget17.4 ± 0.917.5 ± 0.618.02 ± 0.6617.68 ± 0.49Open in a separate window*Values calculated from data presented in tables and text in Schauffler et al. (26, 27).Open in a separate windowFig. S5.Vertical profiles of halons, CH3Br, and VSLorg. (A) Western Pacific (B) Eastern Pacific. Solid marks represent the 1-km bin average of GWAS measurements ±1 SD. Solid lines represent the average from CAM-Chem model with shaded ±1 SD limits.We calculated that, during ATTREX, the average level of measured bromine resulted in 20% of total ozone destruction in the tropical lower stratosphere. However, potential changes in the ocean−air flux or a rise in seaweed cultivation could increase VSLorg emissions, leading to an even larger percentage of ozone depletion. Further observations with high-altitude aircraft will improve our understanding of the role of VSLorg in the composition of the tropopause region and the processes occurring in the TTL, diminish the uncertainties of the amount of Bry that enters the stratosphere, and ascertain whether VSLBr is changing in this critical region.  相似文献   
10.
Pulmonary arteriovenous malformations: techniques and long-term outcome of embolotherapy   总被引:23,自引:0,他引:23  
White  RI  Jr; Lynch-Nyhan  A; Terry  P; Buescher  PC; Farmlett  EJ; Charnas  L; Shuman  K; Kim  W; Kinnison  M; Mitchell  SE 《Radiology》1988,169(3):663-669
Over a 10-year period, 276 pulmonary arteriovenous malformations (PAVMs) were occluded with balloon embolotherapy in 76 patients, 67 (88%) of whom had hereditary hemorrhagic telangiectasia. Eleven patients (14%) were discovered by means of family screening with measurement of arterial blood gases and chest radiography. Epistaxis, dyspnea, hemoptysis, and hemothorax occurred in 79%, 71%, 13%, and 9% of patients, respectively. Clinical histories of strokes and transient ischemic attacks were present in 18% and 37% of patients, respectively. Computed tomographic scans of 59 patients showed stroke in 36%. Sixty-five percent of PAVMs were located in the lower lobes, which correlated with the finding of more pronounced hypoxemia in the upright position. After embolotherapy, symptomatic hypoxemia was corrected, and serial values have remained constant for 5 years. Complications were minimal, and no patient required surgery. Balloon embolotherapy is effective long-term therapy for PAVMs, and family screening should be pursued because of the possibility of a higher frequency of paradoxical embolization (stroke) than previously recognized.  相似文献   
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