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11.

Objectives

The aim of this study was to investigate possible predictors of irrational parenthood cognitions among infertile women seeking treatment.

Methods

In a cross-sectional study, 300 women who visited an Infertility Center in Iran during 2010 were studied. A pre-validated inventory was used to assess irrational parenthood cognitions. Potential predictors of the total irrational parenthood cognitions score were assessed.

Results

Mean irrational parenthood cognition score was 39.7(Range 0–56). Through bivariate analysis, the score on irrational parenthood cognition was inversely correlated with age and positively correlated with length of time seeking for infertility treatment and length of time expecting pregnancy. In a multivariate model, infertile women with higher education, especially academic education, or those with higher economic status were less likely to have irrational parenthood cognitions. However, higher motherhood motivation, no previous experience of pregnancy and being under social pressure, from others around, increased the likelihood of having irrational parenthood cognitions.

Conclusions

Some variables such as female spouse’s educational level and being under social pressure can independently predict irrational parenthood cognitions among infertile women that may be of use in designing health promotion plans in order to target the vulnerable women.  相似文献   
12.

Fe20:Ag80, Fe50:Ag50, and Fe80:Ag20 bimetallic nanoparticles were prepared with laser ablation method applied on Fe/Ag/polyvinyl alcohol (PVA) composite, at two different ablation times (20 and 50 min). The ratio of Fe with respect to Ag atoms as well as ablation time affect wavelength, intensity, and width of plasmon absorption peak. Increase in Fe content leaded to a redshift and a decrease in intensity and an increase in the width of plasmon absorption peaks. The transmission electron microscopy (TEM) analysis showed three kinds of grains which are Ag nanoparticles, Ag/Fe core/shells and Fe nanoparticles. Due to the concentration of Fe nanoparticles with the size of less than 5 nm around Ag ones with the size of 20 to 30 nm, a core–shell structure of these two metals forms and this decreases Ag plasmon resonance frequency, and as a result, its absorption peak has a redshift. According to the results of vibrating sample magnetometer (VSM), the Fe/Ag bimetallic nanoparticles were superparamagnetic.

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13.
Obesity, especially when complicated with hypertension, is associated with structural and functional cardiac changes. Recent studies have focused on the prognostic impact of the type of left ventricular (LV) geometric remodeling. This study looked at the prevalence and clinical correlates of LV geometric patterns and their relation to cardiac function in a sample of predominantly African‐American (AA) youth. Echocardiographic data was collected on 213 obese (BMI of 36.53 ± 0.53 kg/m2) and 130 normal‐weight subjects (BMI of 19.73 ± 0.21 kg/m2). The obese subjects had significantly higher LV mass index (LVMI; 49.6 ± 0.9 vs. 46.0 ± 1.0 g/m2.7, P = 0.01), relative wall thickness (RWT; 0.45 ± 0.00 vs. 0.40 ± 0.00, P < 0.001), left atrial (LA) index (33.2 ± 0.7 vs. 23.5 ± 0.6 ml/m, P < 0.001), more abnormal diastolic function by tissue Doppler E/Ea septal (7.5 ± 0.14 vs. 6.5 ± 0.12 ms, P < 0.001), E/Ea lateral (5.7 ± 0.12 vs. 4.8 ± 0.1 ms, P < 0.001), myocardial performance index (MPI; 0.43 ± 0.00 vs. 0.38 ± 0.00, P < 0.001), and Doppler mitral EA ratio (2.0 ± 0.04 vs. 2.4 ± 0.07, P < 0.001) but similar systolic function. Concentric remodeling (CR) was the most prevalent pattern noted in the obese group and concentric hypertrophy (CH) in the obese and hypertensive group. Obesity, hypertension, and CH were independent predictor of diastolic dysfunction. Systolic (SBP) and diastolic blood pressures (DBP) were the prime mediators for CH whereas obesity and diastolic blood pressure were predictors of CR. No significant association was observed between the geometric patterns and systolic function. Tracking LV hypertrophy (LVH) status and geometric adaptations in obesity may be prognostic tools for assessing cardiac risk and therapeutic end points with weight loss.  相似文献   
14.
Teoh  Chia Pei  Laya  Juan Carlos 《Facies》2021,67(4):1-31
Facies - The late Aptian Lower Serdj Formation (LSF) in the Northern Atlas of Tunisia records a mixed carbonate–siliciclastic system from the southern margin of Tethys. Sedimentological...  相似文献   
15.
The Early Cretaceous Fort Terrett Formation of Mason County, central Texas, is a succession of subtidal to peritidal mud-dominated facies with minor intervals of bioclastic packstone–grainstone, rudist floatstone, and interbedded chert nodules. The strata conformably overlie the Hensel Formation, which was deposited unconformably on Precambrian basement. The Hensel Formation also contains a significant percentage of dolomite, precipitated within a fine-grained clayey matrix. The Hensel and Fort Terrett Formations were deposited during a transgressive episode, which provided the conditions for the extensive shallow-water Comanche carbonate platform. Siliciclastic and carbonate sediments were deposited along the coastal margin in subtidal, intertidal to supratidal areas. Previous dolomitization models have suggested that high permeability layers are required for dolomitizing brines to flow through a carbonate succession. Although, interparticle porosity in muddy tidal-flat successions can be significant, it has a limited flow capacity. However, interconnected fenestral porosity can allow sufficient fluid flow to move dolomitizing fluids more efficiently through the succession. Thus, it is hypothesized that interconnected fenestral porosity could have had a significant impact on permeability within this muddy succession and provided the pathways and conduits for Mg-rich brines. Four types of dolomite are recognized in the Fort Terrett succession. Three of these dolomite types formed largely by replacement and they occur throughout the succession. Features such as crystal size, crystal face geometry and zonation reflect the progressive development and recrystallization of the dolomite types. Only type 4 dolomite formed as a cement in void spaces during a late diagenetic stage. The direction of the dolomitizing fluid movement is difficult to determine, but it was likely downward in this case, controlled by a density-head driving-mechanism generated by dense hypersaline fluids from an evaporating lagoon.  相似文献   
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