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61.
Dominant mutations in two functionally related DNA/RNA-binding proteins, trans-activating response region (TAR) DNA-binding protein with a molecular mass of 43 KDa (TDP-43) and fused in sarcoma/translocation in liposarcoma (FUS/TLS), cause an inherited form of ALS that is accompanied by nuclear and cytoplasmic aggregates containing TDP-43 or FUS/TLS. Using isogenic cell lines expressing wild-type or ALS-linked TDP-43 mutants and fibroblasts from a human patient, pulse-chase radiolabeling of newly synthesized proteins is used to determine, surprisingly, that ALS-linked TDP-43 mutant polypeptides are more stable than wild-type TDP-43. Tandem-affinity purification and quantitative mass spectrometry are used to identify TDP-43 complexes not only with heterogeneous nuclear ribonucleoproteins family proteins, as expected, but also with components of Drosha microprocessor complexes, consistent with roles for TDP-43 in both mRNA processing and microRNA biogenesis. A fraction of TDP-43 is shown to be complexed with FUS/TLS, an interaction substantially enhanced by TDP-43 mutants. Taken together, abnormal stability of mutant TDP-43 and its enhanced binding to normal FUS/TLS imply a convergence of pathogenic pathways from mutant TDP-43 and FUS/TLS in ALS.  相似文献   
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BACKGROUND: Procalcitonin (PCT) is a biomarker for the diagnosis of sepsis and bacterial infection diseases. METHODS: A new fully automated SphereLight PCT (SL-PCT) assay system for PCT concentration in human serum or plasma by using SphereLight 180 (SL180, Olympus Corp.) analyzer was developed. The SL-PCT assay is based on chemiluminescent enzyme immunoassay. RESULTS: A linear dose response relationship was observed up to 200 ng/ml PCT concentration. The detection limit of PCT concentration was 0.06 ng/ml. Endogenous substances, anticoagulants, sodium fluoride and drugs did not interfere with assay results. There was a good correlation between the present method and the manual method in serum and plasma samples. CONCLUSIONS: These results indicate that the SL-PCT assay showed good performance in terms of the linearity, detection limit and precision. Use of this PCT measurement may improve the detection of sepsis and infectious disease.  相似文献   
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Among pancreatic neoplasms, pancreatic schwannoma is quite rare. We report a case of solitary pancreatic schwannoma, plus a literature review of this tumor. A 71-year-old woman was diagnosed by abdominal ultrasonography as having a pancreatic tumor and was hospitalized in our department at Kumamoto University Hospital on January 26, 2006. Abdominal computed tomography, magnetic resonance imaging, and endoscopic ultrasonography all showed this tumor, which was located in the body of the pancreas, to have cystic and solid components, and with a septum in the cystic part of the lesion. The tumor, preoperatively identified as a mucinous cystic neoplasm, was clearly separated from the normal pancreatic parenchyma. We performed a spleen-preserving distal pancreatectomy with a lymph node dissection on February 7, 2006. A histopathological examination of the resected specimen by means of hematoxylin and eosin revealed the tumor to consist of two parts: one with a compact spindle cell pattern (Antoni type A), and the other showing degeneration of fat (Antoni type B). We also found positive results for immunohistochemical staining for S-100 and vimentin. These findings confirmed the tumor’s classification as a pancreatic schwannoma.  相似文献   
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Several animal and human studies suggest pharmacological approaches may prevent steroid-induced osteonecrosis (ON). We asked whether the newly developed 3-hydroxymethyl-3-glutaryl-CoA (HMG-CoA) reductase inhibitor, pitavastatin, could prevent steroid-induced ON in rabbits. We injected 65 adult male Japanese white rabbits once with 20 mg/kg of methylprednisolone acetate into the right gluteus medius muscle. The rabbits were divided into two groups; one group of 35 rabbits received pitavastatins (PS), and the other group of 30 rabbits received no prophylaxis (CTR). Hematological examinations were performed just before the steroid injection (0 weeks) and at 1 and 2 weeks after steroid injection; both the femora and the humeri were histologically examined 2 weeks postinjection. The incidence of histologic changes consistent with early ON in the PS group (13 of 35; 37%) was lower in comparison to the CTR group (21 of 30; 70%). The size of the bone marrow fat cells in the PS group (56.6 +/- 10 microm) was smaller than those in the CTR group (60 +/- 4 microm). The data suggest pitavastatin has the potential to lower the incidence of steroid-induced ON in rabbits.  相似文献   
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AIM/METHODS: Diabetic nodular glomerulosclerosis is considered to be the specific renal lesion of diabetes mellitus (DM). However, some cases, in which nodular glomerulosclerosis was found without any manifestation of DM, have also occasionally been reported. We clinicopathologically examined seven cases without a prior history of DM. They consisted of six men and one woman with a mean age of 57 years, and included three cases with family history of DM and six cases with hypertension. RESULTS: Mean body mass index was 26.2 +/- 5.9 (means +/- SD) kg/m(2) and haemoglobin A1c 5.3 +/- 1.1% or haemoglobin A1 7.0 +/- 0.6%. Mean plasma glucose levels were 5.3 +/- 0.7 mmol/L at fasting and 10.1 +/- 1.9 mmol/L at 2 h of 75 g OGTT (normal: 1 patient; impaired glucose tolerance: 4 patients; DM: 2 patients). None of them showed diabetic retinopathy in fundoscopic ophthalmoscopy. Mean serum creatinine was 268 +/- 215 micromol/L, urinary protein 5.2 +/- 4.0 g/day, and three patients had mild haematuria. Renal biopsy revealed typical nodular glomerulosclerosis, a negative deposition based on an immunofluorescence study, and neither any significant electron dense deposits nor fibrils on electron microscopy. CONCLUSION: These patients at presentation had no overt clinical manifestations of glucose intolerance. Diabetic nodular glomerulosclerosis can occur in patients without overt DM, suggesting the role of factors additional to prolonged hyperglycaemia in the pathogenesis of this disorder.  相似文献   
68.
It has been shown that dietary polyunsaturated fatty acids stimulate the liver microsomal mixed function oxidase system. The influence of different levels of dietary lard, soybean oil and sardine oil on the mixed function oxidase system was investigated in rats. The diet containing 5% sardine oil rich in eicosapentaenoic and docosahexaenoic acids stimulated the mixed function oxidase system, but the diet containing 5% lard in which lard consisted of 10.7% linolenic acid and 1.5% linolenic acid seemed unlikely to stimulate enough the mixed function oxidase system. On the other hand, no definite effects of large doses of dietary lipids, 25% in the diets, on the mixed function oxidase system were observed.  相似文献   
69.
Using the Japan Meteorological Agency earthquake catalog, we investigate the seismicity variations before major earthquakes in the Japanese region. We apply natural time, the new time frame, for calculating the fluctuations, termed β, of a certain parameter of seismicity, termed κ1. In an earlier study, we found that β calculated for the entire Japanese region showed a minimum a few months before the shallow major earthquakes (magnitude larger than 7.6) that occurred in the region during the period from 1 January 1984 to 11 March 2011. In this study, by dividing the Japanese region into small areas, we carry out the β calculation on them. It was found that some small areas show β minimum almost simultaneously with the large area and such small areas clustered within a few hundred kilometers from the actual epicenter of the related main shocks. These results suggest that the present approach may help estimation of the epicentral location of forthcoming major earthquakes.In this study, we investigate the evolution of seismicity shortly before main shocks in the Japanese region, N2546E125148, using Japan Meteorological Agency (JMA) earthquake catalog as in ref 1. For this, we adopted the new time frame called natural time since our previous works using this time frame made the lead time of prediction as short as a few days (see below). For a time series comprising N earthquakes (EQs), the natural time χk is defined as χkk/N, where k means the kth EQ with energy Qk (Fig. 1). Thus, the raw data for our investigation, to be read from the earthquake catalog, are χkk/N and pk=Qk/n=1NQn, where pk is the normalized energy. In natural time, we are interested in the order and energy of events but not in the time intervals between events.Open in a separate windowFig. 1.EQ sequence in (A) conventional time and (B) natural time. In B, Qk is given in units of the energy ε corresponding to a 3.5MJMA EQ.We first calculate a parameter called κ1, which is defined as follows (2, 3), from the catalog.κ1=k=1Npkχk2(k=1Npkχk)2=χ2χ2.[1]We start the calculation of κ1 at the time of initiation of Seismic Electric Signals (SES), the transient changes of the electric field of Earth that have long been successfully used for short-term EQ prediction (4, 5). The area to suffer a main shock is estimated on the basis of the selectivity map (4, 5) of the station that recorded the corresponding SES. Thus, we now have an area in which we count the small EQs of magnitude greater than or equal to a certain magnitude threshold that occur after the initiation of the SES. We then form time series of seismic events in natural time for this area each time a small EQ occurs, in other words, when the number of the events increases by one. The κ1 value for each time series is computed for the pairs (χk,pk) by considering that χk is “rescaled” to χk = k/(N +1) together with rescaling pk=Qk/n=1N+1Qn upon the occurrence of any additional event in the area. The resulting number of thus computed κ1 values is usually of the order 102 to 103 depending, of course, on the magnitude threshold adopted for the events that occurred after the SES initiation until the main shock occurrence. When we followed this procedure, it was found empirically that the values of κ1 converge to 0.07 a few days before main shocks. Thus, by using the date of convergence to 0.07 for prediction, the lead times, which were a few months to a few weeks or so by SES data alone, were made, although empirically, as short as a few days (6, 7). In fact, the prominent seismic swarm activity in 2000 in the Izu Island region, Japan, was preceded by a pronounced SES activity 2 mo before it, and the approach of κ1 to 0.07 was found a few days before the swarm onset (8). However, when SES data are not available, which is usually the case, it is not possible to follow the above procedure. To cope with this difficulty, in the previous work (1), we investigated the time change of the fluctuation of the κ1 values during a few preseismic months for each EQ (which we call target EQ) over the large area N2546E125148 (Fig. 2A) for the period from 1 January 1984 to 11 March 2011, the day of M9.0 Tohoku EQ. Setting a threshold MJMA = 3.5 to assure data completeness of JMA catalog, we were left with 47,204 EQs in the concerned period of about 326 mo: ∼150 EQs per month. For calculating the β values, we chose 200 EQs before target EQs to cover the seismicity in almost one and a half months.Open in a separate windowFig. 2.(A) The 47,204 EQs with MJMA ≥ 3.5 that occurred during the period of our study. (B) Contours of the number of EQs per month within R = 250 km. Solid diamonds show the epicenters of six shallow EQs investigated in this study. (C) Contours of the natural time window W used in each of the 12,476 areas of radius R = 250 km with offset 0.1° from one another that have at least eight EQs per month.To obtain the fluctuation β of κ1, we need many values of κ1 for each target EQ. For this purpose, we first took an excerpt comprised of W successive EQs just before a target EQ from the seismic catalog. The number W was chosen to cover a period of a few months. For this excerpt, we form its subexcerpts Sj={Qj+k1}k=1,2,,N of consecutive N = 6 EQs (since at least six EQs are needed (2) for obtaining reliable κ1) of energy Qj+k?1 and natural time χkk/N each. Further, pk=Qj+k1/k=1NQj+k1, and by sliding Sj over the excerpt of W EQs, j=1,2,,WN+1 (= W − 5), we calculate κ1 using Eq. 1 for each j. We repeat this calculation for N=7,8,,W, thus obtaining an ensemble of [(W − 4)(W − 5)]/2 (= 1 + 2 +…+ W − 5) κ1 values. Then, we compute the average μ(κ1) and the SD σ(κ1) of thus obtained ensemble of [(W − 4)(W − 5)]/2 κ1 values. The variability β of κ1 for this excerpt W is defined to be β ≡ σ(κ1)/μ(κ1) and is assigned to the (W + 1)th EQ, i.e., the target EQ.The time evolution of the β value can be pursued by sliding the excerpt through the EQ catalog. Namely, through the same process as above, β values assigned to (W + 2)th, (W + 3)th, … EQs in the catalog can be obtained.We found in ref. 1 that the fluctuation β of κ1 values exhibited minimum a few months before all of the six shallow EQs of magnitude larger than 7.6 that occurred in the study period. A minimum of β ≡ σ(κ1)/μ(κ1) means large average and/or small deviation of κ1 values (e.g., see ref. 9).In the present work, we calculate the β values for small areas before the six large EQs, which showed β minima of the large area.  相似文献   
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