scholarly journals SAMANYA SHODHANA OF RAW VANGA BY DHALANA METHOD WITH SPECIAL REFERENCE TO RASTARANGINI: PHARMACEUTICO-ANALYTICAL STUDY FROM ASHVIN RURAL AYURVED COLLEGE, MANCHIHILL, SANGAMNER, MAHARASHTRA

2020 ◽  
Vol 8 (7) ◽  
pp. 3886-3889
Author(s):  
Supriya A. Giri ◽  
Ravindra Atram ◽  
Smita Kolte ◽  
Sanjeev Lokhande

Background: Shodhana is a process which separate mala by doing Peshana, Khalana, Mardana, Dhala-na, Nirvapana, Swedhana etc. Objective: To study the physical, chemical changes in raw Vanga before and after Samanya Shodhana. Materials & Methods: In the present study, Vanga Shodhana is carried out by Dhalana method in different media as Taila, Takra, Gomutra, Aranala, Kulattha Kwatha for 7 times. Results and Conclusions: Physical changes take place in metal useful for further process. Removal of zinc and lead from the raw Vanga shows the importance of Malavicchedana property of Shodhana. Vanga un-dergoes the oxidation as a chemical change which quickens the further process of Jarana and Marana

2021 ◽  
Vol 14 (1) ◽  
pp. 243
Author(s):  
Soo-Young Moon ◽  
Hyeon Soo Kim ◽  
Daehee Jang ◽  
Ji-Young Lee

This study investigates the soil chemical changes and crop growth characteristics after treatment with carbonized tangerines prepared using plasma. To determine the effect of the carbonized tangerines on crop, four test plots were treated with chaff charcoal or different ratios of coco peat and carbonized tangerines. Lettuce was grown on the plots, and the chemical changes in soil and physical changes in the lettuce were observed. Chemical changes in the soil before and after the carbonized tangerine treatments were very similar to those before and after chaff charcoal treatment. Lettuce leaf length, width, weight, and count in carbonized tangerine-treated plots significantly increased than those in the untreated plot. Our results found that the carbonization of tangerines using plasma can be a good alternative for processing many by-products generated during cultivation. In addition, the possibility of using carbonized tangerines as biochar has been explored.


2021 ◽  
Author(s):  
João Victor de Araújo Souza ◽  
Monalisa Silva de França ◽  
Nayara Karina Ferreira Pereira ◽  
Denise Soares de Araújo ◽  
Roberta de Oliveira Cacho ◽  
...  

Introduction: Stroke is a major cause of death and mortality worldwide. The sedentary lifestyle is a modifiable risk factor and the regular practice of physical activity can reduce the recurrence of stroke and its symptoms. Objective: To characterize the level of physical activity of post-stroke patients before and after the event. Methodology: This is a cross-sectional, analytical study. The population of the study consisted of patients diagnosed with stroke, in the chronic phase under treatment or that have already been discharged from the Physiotherapy School Clinic of FACISA in Santa Cruz-RN. The individuals were evaluated by the Modified Baecker Questionnaire for the Elderly (QBMI) that classifies the level of physical activity in: sedentary (-9), active (9 to 16), and athletes (+16). The normality of the variables was verified by the Shapiro-Wilk test. Wilcoxon’s test was used for comparative analysis of QBMI before and after stroke. Results: Nineteen patients participated (8 male and 11 female) with a mean age of 63 years, of these, 11 had systemic hypertension. Before, 3 were classified as sedentary (score mean: 5.34), 5 active (score mean: 12.254) and 1 athlete ( score mean: 27.04). After the stroke, 18 were classified as sedentary (score mean: 1.46) (p=0.001). Conclusion: There was a reduction in the participants’ level of physical activity, showing greater sedentariness after stroke, although physical activity is essential for secondary prevention of stroke.


2021 ◽  
pp. SP520-2021-52
Author(s):  
Young Kwan Sohn ◽  
Chanwoo Sohn ◽  
Woo Seok Yoon ◽  
Jong Ok Jeong ◽  
Seok-Hoon Yoon ◽  
...  

AbstractThe Holocene tuff ring of Songaksan, Jeju Island, Korea, is intercalated with wave-worked deposits at the base and in the middle parts of the tuff sequence, which are interpreted to have resulted from fair-weather wave action at the beginning of the eruption and storm wave action during a storm surge event in the middle of the eruption, respectively. The tuff ring is overlain by another marine volcaniclastic formation, suggesting erosion and reworking by marine processes because of post-eruption changes of the sea level. Dramatic changes of the chemistry, accidental componentry, and ash-accretion texture of the pyroclasts are also observed between the tuff beds deposited before and after the storm invasion. The ascent of a new magma batch, related to the chemical change, could not be linked with either the Earth and ocean tides or the meteorological event. However, the changes of the pyroclasts texture suggest a sudden change of the diatreme fill from water-undersaturated to supersaturated because of an increased supply of external water into the diatreme. Heavy rainfall associated with the storm is inferred to have changed the water saturation in the diatreme. Songaksan demonstrates that there was intimate interaction between the volcano and the environment.


PROMINE ◽  
2018 ◽  
Vol 6 (2) ◽  
pp. 16-23
Author(s):  
Harnani .

Water pollution is a thing that can affect the environment, especially on health and hygiene environment around. Sub Keluang Regency Musi Betung South Sumatra known to have oil drilling wells of the Earth where illegal do not fit a common standardization is done, so worried about polluted areas the surroundings. This research aims to study and know the impact of environmental pollution due to the illegal drilling by local people, as well as provide information research results to the Government and the police to cooperate in enforcing laws that have set. To find out which level contamination using a research method that is mapping rivers and wells include deskipsi the physical characteristics, such as water color, flavor, odor, retrieval example of a sample for the analysis of physical-chemical content of the water, and the projection of the level of public health. The result of the physical identification of the water as much as 8 samples were declared contaminated. Sampling see the provisions on physical changes on either the river or the well, the results of the analysis of physical-chemical water, found many chemical compounds which exceed standard pH obtained ranged from 6.25- 8.16 and types of groundwater salt (31-464 mg/L TDS), increase the value of pH and TDS is assumed to be due to saltwater waste results from drilling for petroleum is illegal, and the presence of chemical compounds, either the main or excessive accessories in water then it can affect health, which that is evidenced by the results of the projection of the level of public health from the years 2016 to now that continues to decline. referring to the decision of the Minister of State for the environment number: 115 the year 2003 on guidelines for the determination of the Status of Water quality by the State Minister for the environment using STORET method with a score of 16 (polluted medium).


1897 ◽  
Vol 21 ◽  
pp. 25-34
Author(s):  
W. N. Hartley

In Nature of January 24, 1895, appears an abstract of a paper read before the Royal Society of Edinburgh on March 7, 1892, by Dr John Murray and Mr Robert Irvine, and published in the Transactions of the Society, vol. xxxvii. part 2, No. 23, entitled “Chemical Changes between Sea-water and Oceanic Deposits.”This is an account of a chemical examination of the sea-water salts in the water adhering to or retained in mud, with special reference to the formation of the deposit known as “Blue Mud.”Dittmar's analysis of sea-water is quoted and compared with an analysis of mud-water. The chief points of difference between the two is the occurrence in mud-water salts of 0·206 per cent. of ammonium sulphate, 0·729 per cent. of magnesium carbonate, and 0·18 per cent. of manganous carbonate; also that the total salts are low in proportion to the chlorine they contain.The occurrence of ammonium sulphate in this mud, and also of manganous carbonate, are facts of much interest; but there are some equations given to explain the chemical changes which the mud undergoes which are not strictly in accordance with facts. There are three points which I would desire to draw attention to: first, the reduction of the sulphates; second, the oxidation of sulphuretted hydrogen; and third, the formation of manganous carbonate.The equations are written without reference to the part played by water in the chemical changes involved, but it may have been thought that the accuracy sacrificed was compensated by the simpler form of the equations.


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