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Objective To explore the correlations between different traditional Chinese medicine (TCM) syndromes and the heart rate variability (HRV) accompanying patients with chest pain,and to provide a referen()for clinical syndrome differentiation in such patients.Methods A prospective study was conducted.()hundred and seventeen patients with chest pain admitted into Longhua Hospital Affiliated to Shanghai U()of TCM from January 2015 to October 2016 were assigned in a study object,and according to the diffe()TCM syndromes,they were divided into syndrome of qi deficiency with blood stasis,the blood sta()the deficiency of qi and yin,suppression of the chest yang,phlegm and blood stasis,qi-stagnan ()syndromes.In the same period,123 healthy people having undergone physical examination wer()control group.The time domain indexes of HRV were recorded by dynamic electrocardiogr()normal control group were compared to those of patients with different TCM syndrom()distribution in different TCM syndromes and various HRV time domain indexes we()cycle time domain indexes were as follows:the average standard deviation o()standard deviation of R-R interval (SDNN),24 hours standard deviation of()5 minutes (SDANN),24 hours the mean square root of difference values,()were observed in both groups.Results The chest pain patients a()accounting for the largest proportion (35 cases,29.9％),and ac()smallest proportion (5 cases,4.3％) in the study group;the nu()syndrome (17 cases vs.14 cases),blood stagnation of hea()(6 cases vs.2 cases) and qi-stagnation and blood stasis s()in men;the numbers of patients with deficiency of qi()(4 cases vs.2 cases) in men were more than thos()female patients were lower than those in maj()66.8 (33.4,33.4) vs.103.4 (39.7,135.4),124.7 (88.0,143.4) vs.167.0 (90.5,230.1),84.0 (22.5,132.6) vs.152.4 (31.4,240.0),all P ＜ 0.05].The SDANN in patients with chest discomfort accompanied by any one of the above mentioned types of TCM syndrome was significantly lower than that in the control group,and its degree of descent was more remarkable in the patients with qi deficiency with blood stasis,the blood stagnation of heart and suppression of the chest yang syndromes (ms:74.86± 25.69,80.39± 20.53,70.97± 23.53 vs.131.30± 34.70,all P ＜ 0.05);the SDNN of patients with deficiency of qi and yin syndrome was higher than that in the blood stagnation of heart syndrome,phlegm and blood stasis,and qi-stagnation and blood stasis syndrome significantly (ms:181.25 ± 65.20 vs.97.88± 23.61,84.28 ± 22.34,89.93 ± 8.43,all P ＜ 0.05);the RMSSD of patients with deficiency of qi and yin syndrome was increased significantly compared with that in the healthy controls and in patients with the blood stagnation of heart syndrome (ms:91.94 ± 44.02 vs.28.00± 10.50,32.21 ± 18.25,both P ＜ 0.05).Conclusions Patients with chest pain accompanied by different TCM syndrome types may develop obvious heart rate variability,and the descent of SDANN level was the most significant.The analysis of HRV changes in such patients has positive significance for their diagnosis and treatment.
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Objective To investigate the clinical effects of different dosages of Shenfu injection for treatment of elderly patients with refractory chronic congestive heart failure (CHF).Methods A prospective study was conducted, 360 patients with CHF from Longhua Hospital Affiliated to Shanghai University of Traditional Chinese Medicine were enrolled, and they were randomly divided into low dose, middle dose and high dose Shenfu injection groups. In the three groups, the patients received the same conventional medicine therapy, and additionally they were treated by low, medium and high dose Shenfu injection (60, 80, 100 mL/d, respectively), once a day. The therapeutic course was 10 days in the three groups. After treatment, the clinic therapeutic effect, left ventricular diastolic end diameter (LVEDD), left ventricular ejection fraction (LVEF), stroke volume (SV), cardiac output (CO), cardiac index (CI) and plasma B type natriuretic peptide (BNP) were observed in the three groups.Results The total therapeutic effective rate in middle dose Shenfu injection group was significantly higher than that in low dose and high dose Shenfu injection groups [82.5% (99/120) vs. 54.2% (65/120), 60.0% (72/120), bothP < 0.05]. In high dose Shenfu injection group, increase of blood pressure occurred in 15 cases (12.5%), but no such phenomenon appeared in low and middle dose Shenfu injection groups. In the three groups, no cardiac arrhythmia, liver function abnormality, myocardial enzymogram abnormality, etc. adverse reactions occurred. Compared with those before treatment, after treatment in three groups the LVEDD and BNP were significantly decreased, while LVEF, SV, CO and CI were markedly increased. The changes of above index in middle dose Shenfu injection group were more significant [LVEDD (mm): 46.1±6.3 vs. 58.3±4.4; LVEF: 0.561±0.056 vs. 0.324±0.044, SV (mL): 58.1±6.3 vs. 35.7±5.4, CO (L/min): 5.78±0.60 vs. 4.21±0.78, CI (mL·s-1·m-2): 81.85±7.33 vs. 53.01±9.00, BNP (ng/L): 355.4±76.6 vs. 3 263.2±65.7, allP < 0.05]. Conclusion Shenfu injection 80 mL/d is the best effective dosage for treatment of elderly patients with refractory CHF and its incidence of adverse events is low.
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The Water-Sediment Regulation Scheme (WSRS) of the Yellow River is a procedure implemented annually from June to July to expel sediments deposited in Xiaolangdi and other large middle-reach reservoirs and to scour the lower reaches of the river, by controlling water and sediment discharges. Dissolved uranium isotopes were measured in river waters collected monthly as well as daily during the 2010 WSRS (June 19-July 16) from Station Lijin (a hydrologic station nearest to the Yellow River estuary). The monthly samples showed dissolved uranium concentrations of 3.85-7.57 µg l(-1) and (234)U/(238)U activity ratios of 1.24-1.53. The concentrations were much higher than those reported for other global major rivers, and showed seasonal variability. Laboratory simulation experiments showed significant uranium release from bottom and suspended sediment. The uranium concentrations and activity ratios differed during the two stages of the WSRS, which may reflect desorption/dissolution of uranium from suspended river sediments of different origins. An annual flux of dissolved uranium of 1.04 × 10(8) g y(-1) was estimated based on the monthly average water discharge and dissolved uranium concentration in the lower reaches of the Yellow River. The amount of dissolved uranium (2.65 × 10(7) g) transported from the Yellow River to the sea during the WSRS constituted about 1/4 of the annual flux.