scholarly journals Signs of gathering and fishing on the monuments of the Late Neolithic - Early Eneolithic of Karelia (based on the settlement of Vigainavolok I)

2019 ◽  
Vol 8 (3) ◽  
pp. 150-157
Author(s):  
Tatyana Anatolyevna Vasilyeva
Keyword(s):  
Large Body ◽  
Climatic Conditions ◽  
Stone Age ◽  
Late Neolithic ◽  
The West ◽  
Forest Zone ◽  
Lake Onega ◽  
Study Results ◽  
Determining Factors

The paper presents the study results of Vigainavolok I materials. This settlement is located on the west of Lake Onega in Karelia. The monument was investigated by G.A. Pankrushev in 1963-1966. Its area was 8,000 m. 26 buildings remains were revealed. The area of 2748 m was studied. The inventory collection includes more than 25 thousand pieces of ceramics and about 7 thousand pieces of stone, clay and metal. The buildings served as dwellings and workshops. The collection includes sinkers that are marked as direct signs of fishing. Favorable climatic conditions for the development in the forest zone, confined to the coast of a large body of water, settlement equipment, osteological materials of the Stone Age monuments characterize fishing as one of the determining factors in the life of the population.

scholarly journals The Association between Ranitidine Use and Gastrointestinal Cancers

Cancers ◽  
2020 ◽  
Vol 13 (1) ◽  
pp. 24
Author(s):  
Gerald McGwin
Keyword(s):  
Adverse Event ◽  
Adverse Events ◽  
Reporting System ◽  
Large Body ◽  
Science Research ◽  
Gastrointestinal System ◽  
Gastrointestinal Cancers ◽  
H2 Antagonists ◽  
Study Results ◽  
Risk Of Cancer

N-nitrosodimethylamine (NDMA) is a carcinogen in experimental animals. It has been classified a probable human carcinogen and has been found in ranitidine. This study sought to evaluate the association between ranitidine use and cancer of the gastrointestinal system. Events reported to the FDA Adverse Events Reporting System that were associated with the use of proton pump inhibitors (PPIs) and H2 antagonists were selected. Proportionate reporting ratios (PRRs) and associated 95% confidence intervals (CIs) were calculated to compare the proportion of all reported adverse events that were for gastrointestinal system cancers among adverse event reports for ranitidine to adverse event reports for other H2 antagonists. The proportion of adverse events for any gastrointestinal system cancer relative to all other events was elevated for ranitidine compared to PPIs and other H2 antagonists (PRR 3.66, 95% CI 3.19–4.20). Elevated and significant PRRs were observed for pharyngeal (PRR 9.24), esophageal (PRR 3.56), stomach (PRR 1.48), colorectal (PRR 16.31), liver (PRR 2.64), and pancreatic (PRR 2.18) cancers. The PRRs for anal (PRR 4.62) and gallbladder (PRR 4.62) cancer were also elevated though not statistically significant. In conjunction with a large body of epidemiologic and human and animal basic science research, the study results support the hypothesis that NDMA-contaminated ranitidine increases the risk of cancer and supports the withdrawal of these medications from the market.

Late-glacial and Post-glacial history of the Chalk escarpment near Brook, Kent

1964 ◽  
Vol 248 (745) ◽  
pp. 135-204 ◽  
Keyword(s):  
Bronze Age ◽  
Iron Age ◽  
Late Glacial ◽  
Climatic Conditions ◽  
Valley Floor ◽  
Glacial Period ◽  
Late Neolithic ◽  
Local Conditions ◽  
Arable Farming ◽  
History Of

This paper describes the morphology of a small piece of the Chalk escarpment near Brook in east Kent, and reconstructs its history since the end of the Last Glaciation. The escarpment contains a number of steep-sided valleys, or coombes, with which are associated deposits of chalk debris, filling their bottoms and extending as fans over the Gault Clay plain beyond. Here the fans overlie radiocarbon-dated marsh deposits of zone II (10 000 to 8800 B.C.) of the Late-glacial Period. The debris fans were formed and the coombes were cut very largely during the succeeding zone III (8800 to 8300 B.C.). The fans are the products of frost-shattering, probably transported by a combination of niveo-fluvial action and the release of spring waters; intercalated seams of loess also occur. The molluscs and plants preserved in the Late-glacial deposits give a fairly detailed picture of local conditions. The later history of one of the coombes, the Devil’s Kneadingtrough, is reconstructed. The springs have effected virtually no erosion and have probably always emerged more or less in their present position. In the floor of the coombe the periglacial chalk rubbles of zone III are covered by Postglacial deposits, mainly hillwashes. They are oxidized and yield no pollen, but contain rich faunas of land Mollusca, which are presented in the form of histograms revealing changing local ecological and climatic conditions. During most of the Post-glacial Period, from the end of zone III until about the beginning of zone VIII, very little accumulation took place on the coombe floor. But below the springs there are marsh deposits which span much of this interval. They yield faunas of considerable zoogeographical interest. The approximate beginning of zone VII a (Atlantic Period) is reflected by a calcareous tufa, which overlies a weathering horizon, and represents an increase in spring flow. Two clearance phases are deduced from the molluscan record. The first may have taken place at least as early as the Beaker Period (Late Neolithic/earliest Bronze Age); the second is probably of Iron Age ‘A’ date. In Iron Age times the subsoil was mobilized and a phase of rapid hillwashing began. As a result the valley floor became buried by humic chalk muds. The prime cause of this process was probably the beginning of intensive arable farming on the slopes above the coombe; a possible subsidiary factor may have been the Sub-Atlantic worsening of climate. The muds yield pottery ranging in date from Iron Age ‘Kentish first A’ ( ca . 500 to ca . 300 B.C.) to Romano-British ware of the first or second centuries A.D. Evidence is put forward for a possible climatic oscillation from dry to wet taking place at about the time of Christ. In the later stages of cultivation, possibly in the Roman Era, the valley floor was ploughed and given its present-day form.

scholarly journals COMPOSITION, MICROSTRUCTURE AND PROPERTIES OF QUATERNARY CLAYS OF THE PRIKHANKAYSKAYA DEPRESSION (PRIMORYE)

2019 ◽  
Vol 14 (1) ◽  
pp. 20-34
Author(s):  
T. G. RYASHCHENKO ◽  
N. N. UKHOVA ◽  
S. I. SHTELMAKH ◽  
N. I. BELYANINA ◽  
P. S. BELYANIN
Keyword(s):  
Clay Minerals ◽  
Laboratory Data ◽  
Chemical Properties ◽  
Exchange Capacity ◽  
Climatic Conditions ◽  
Water Soluble ◽  
Laboratory Studies ◽  
Microstructural Parameters ◽  
Physical Chemical ◽  
Study Results

The article considers the study results of composition, microstructure and physical-chemical properties of the quaternary clays of the Prikhankayskaya depression in district of the lake Khanka (Primorye) on the example of air-dry samples of geological borehole 45-b in the range of 18–62 m. The objective of research was to obtain new information about the properties of widespread clay sediments in this area using geologic-lithological materials and laboratory data. The schematic geologic-lithological column was composed with the selection of various zones in the quaternary clay sediments section and the border with sediments of the Neogene System. The methodological scheme of laboratory studies of clays was proposed. This scheme includes the determination of chemical and microelement composition, clay minerals, contents of carbonates, water-soluble salts, mobile forms of aluminum oxide, humus, as well as microstructural parameters (method «Microstructure») and some physical-chemical properties. Geochemical coefficients (Kz, CIA, CIW, ICV) determined the degree of chemical maturity of clays and confirmed the results of palynological studies reflecting the fluctuations of the climatic conditions of their formation. For the group of toxic microelements for the first time the special indicator (Zc) was calculated. Which was the criterion for a degree of pollution of the clay sediments section. Clay minerals of the quaternary clays are represented by smectite and hydromica. The clear change in the mineral association was found when passing to the Neogene sediments (kaolinite prevails). The method «Microstructure» revealed the aggregated type of clays microstructure, the domination of the particles of coarse dust fraction among the primary (free) particles and the almost complete absence of the particles of fine-grained sand fraction, the participation of various fractions in the composition of aggregates. The variants of the formation of certain types of aggregates (on sizes) in the fluviolacustrine «khankayskiy» clays are presented. Solid part density, water resistance (soaking time), sedimentation volume, plasticity, relative swelling (samples-pastes) were determined using standard methods for clays. By special methods, the cation exchange capacity was measured and the calculated values of the plasticity index were obtained from forecasting formulas using the yield limit. The proposed methodological scheme of complex laboratory studies of clay sediments can be recommended for problematic geologic-lithological and engineering-geological sections.

scholarly journals KLASIFIKASI SISTEM PEMERINTAHAN (Perspektif Pemerintahan Modern Kekinian)

CosmoGov ◽  
2017 ◽  
Vol 3 (2) ◽  
pp. 148
Author(s):  
Muliadi Anangkota
Keyword(s):  
Theoretical Concept ◽  
Character State ◽  
Parliamentary System ◽  
The Social ◽  
Study Results ◽  
Determining Factors ◽  
Political Conditions ◽  
Descriptive Approach ◽  
The Government

The system of government that practiced in many countries today tend to experience the changes. Some countries have special characteristics of its own in the event of the existence of the country. Characteristic of the country one is to have a system of government. This article is the result of the study the theoretical concept about the classification system of government that until now still practiced in various countries. Study method using the methods of the study of literature with descriptive approach. Study results showed that in the classification of the system of government is currently consists of the parliamentary system, presidential, mixture and a referendum. The system of government to be one of the determining factors in the sustainability of the statehood. On the other the government will run effectively and normal where the old system that is selected and used in accordance with the social political conditions character state.

scholarly journals RESEARCH CONCERNING THE CONTROL OF THE SPECIE Abrosia artemisifolia L.WITH THE HELP OF ERBICIDES

1970 ◽  
Vol 63 ◽  
Author(s):  
N. Hodisan ◽  
G. Morar ◽  
Cornelia Ciobanu
Keyword(s):  
Climatic Conditions ◽  
The West ◽  
Great Production ◽  
Production Losses ◽  
Made In

Recent studies confirms the fact that Abrosia artemisifolia L. sin A.elatior., specie has spread from the west of the country to the central; and south areas, invading agricol crops, provoking great production losses if the intervention in not efficient and made in due time. In the present paper there are presented the effect of several tested herbicides in different phases of vegetation, in climatic conditions of 2006-2007.

scholarly journals Is the indonesian regulation of standard level of service of a pedestrian path fulfill pedestrians’ convenience

2018 ◽  
Vol 147 ◽  
pp. 02003
Author(s):  
Amirotul Mahmudah ◽  
Slamet Legowo ◽  
Agus Sumarsono ◽  
Studyamadyakomunika Linta ◽  
Benny Irawan
Keyword(s):  
User Satisfaction ◽  
Government Regulation ◽  
Level Of Service ◽  
The West ◽  
The North ◽  
Commercial Area ◽  
Movement Characteristics ◽  
Study Results ◽  
Standard Level ◽  
Pedestrian Level Of Service

Indonesia published Regulation No: 03/PRT/M/2014 about the Pedestrian Level of Service (LOS), consist of pedestrian movement characteristics and sidewalk capacity, as like the Bangkok standard, there is no parameter that represents pedestrian interest. Australian standards develop a Level of Service with the main based on categories that relate with pedestrian convenience. Within this study, identifying Indonesian pedestrian interests done by measuring pedestrian perception of convenience. This study aims to check the suitability between this standard pedestrian LOS and pedestrian perception of convenience in a commercial area, Pasar Gede market. The study results, based on Indonesia regulation LOS, the pedestrian path around Pasar Gede market is categorized as level A at all sections, and this is the same as the Bangkok standards. According to the Australian’s standard, the LOS is an A for the West section, B for the North section, and C for the South section. The pedestrians have perceptions of moderately discomfort for all sections. This means that although the pedestrian path fulfills the level of service for Indonesian Government regulation, it does not fulfill user satisfaction. Therefore, the Indonesian LOS standard for pedestrian paths doesn’t provide equity for the pedestrian.

On the issues related to the discoid cores

2017 ◽  
Vol 17 (1) ◽  
pp. 174-178
Author(s):  
Youcheng Chen ◽  
Tongli Qu
Keyword(s):  
Middle Stone Age ◽  
Middle Pleistocene ◽  
Middle Paleolithic ◽  
Stone Age ◽  
The West ◽  
Upper Pleistocene ◽  
Old World ◽  
Insight Into

AbstractThe discoid core and the Levallois core are important symbols of the Middle Paleolithic Age in the west of the Old World. The two types of artifacts show not only technical relationships but also differences. The discoid core can be classified into two sub-types, namely the unifacial and the bifacial classes. In China, discoid cores may have appeared in the upper Middle Pleistocene, and prevailed in the lower and middle Upper Pleistocene, which corresponded to the middle Paleolithic Age in Europe and to the Middle Stone Age in Africa. The discovery and study of discoid cores provide significant insight into the culture of the Middle Paleolithic Age in China.

Investigating Seepage Paths at Golfaraj Earthen Dam, Northwest Iran

2021 ◽  
pp. qjegh2021-053
Author(s):  
Sadegh Saberi Mehr ◽  
Malcolm S. Field
Keyword(s):  
Electrical Conductivity ◽  
Water Level ◽  
Engineering Geology ◽  
Cutoff Wall ◽  
Earthen Dam ◽  
The West ◽  
Reservoir Water ◽  
West Side ◽  
Study Results ◽  
Northwest Iran

An investigation of seepage was conducted at Golfaraj Reservoir Dam with a particular emphasis on determining the seepage areas based on regional and site-specific hydrogeological studies. The primary goal of the investigation was to develop strategies intended to minimize dam and reservoir seepage. Leakage from the reservoir is a serious problem and of considerable concern to the local populace. Substantial reduction of seepage from Golfaraj Reservoir Dam is the ultimate goal of the investigations conducted. Golfaraj Reservoir Dam, located in East Azerbaijan province, northwest Iran, was built to provide water for agricultural and industrial needs in Golfaraj plain and neighboring lands. The Golfaraj Reservoir was constructed through the Miocene Upper Red Formation, which consists of sequences of sandstone, mudstone, conglomerate, and gypsiferous marl. Following reservoir filling, seepage of water into adjacent formations was found to occur at an estimated rate of 70 L/s. After reservoir impoundment groundwater levels in Shahmar village, 2 km downstream and just north of the dam axis, rose and land surfaces became abnormally wet. Lugeon values in some boreholes drilled around Golfaraj Dam before and after dam construction were high enough to indicate that the dam base has sufficient permeability to allow water to escape by underflow. Twenty-four Casagrande piezometers installed around the dam axis at four sectors provided additional information on seepage pathways through the dam body and underneath or through the cutoff wall. Water-level variations in the Casagrande piezometers confirmed the seepage routes. Study results showed that reservoir water likely seeps through the reservoir bottom and beneath and through the cutoff wall. The west side of the dam and near the reservoir reflected water-level rises in accordance with the rise in reservoir-water level. Seepage in this area is probably due to its proximity to Golfaraj Reservoir. Hydrogeochemical analyses further suggest that the water source of Shahmar Drain, ~ 1800 m north of Golfaraj Dam cannot be from the east or west embankments of the dam because the electrical conductivity in Shahmar Drain water approximates the electrical conductivity of Golfaraj Reservoir water and is lower than the electrical conductivity of groundwater in some of boreholes. Potential future seepage mitigation measures will focus on methods to seal the reservoir floor and cutoff wall sections I2-I2 and I3-I3, although some efforts may be directed at the west side of the dam. Such measures could take the form of installation of a geomembrane barrier over the west side of the dam, concrete cutoff walls downstream of the dam, and pumping wells to intercept seepage.Thematic collection: This article is part of the Sustainability in engineering geology and hydrogeology collection available at: https://www.lyellcollection.org/cc/sustainability-in-engineering-geology-and-hydrogeology

The Stone Age in Beechamwell

1913 ◽  
Vol 1 (3) ◽  
pp. 320-321
Author(s):  
R. C. Nightingale
Keyword(s):  
Small Area ◽  
Average Depth ◽  
Stone Age ◽  
The West ◽  
Narrow Strip ◽  
Northern Half ◽  
Top Soil ◽  
Northern Side ◽  
Boulder Clay ◽  
Grey Colour

The greater part of the northern side of the parish of Beechamwell consists of marl and chalk with a top-soil of from one to eighteen feet of gravelly sand. The average depth of this is about eight feet. On the top of it there is a layer of turf or of cultivable soil from three-quarters of a foot to a foot and a-half in depth. There is a narrow strip of boulder clay deposit on which ice-scratched, worked flints are found. There is also a tongue of gravel one and a-half-mile long and half-a-mile wide at its widest part. On this, generally, very few worked flints have been found; fragments of pottery in some numbers have been found all over it however. On the edge of this strip, adjacent on the west to the boulder clay, several worked flints have been picked up, and a hoard of about 200 splinters and flakes was found lying between the sand and the turf, a foot deep here.The greater part of the worked flints are found in an area of about half-a-mile square. The axes, whole or in fragments, are found scattered over the whole of the northern half of the parish. The first axe, however, I found was lying beside a path through the old fen that lies on the south side of Beechamwell. The worked flints found near the moraine are of a peculiar grey colour, and nearly all scimitar-shaped.Flints are found in beds in the chalk and are still plentiful on the surface of the soil, although many have been picked off it for building and road-mending. The small area on which the worked flints are so numerous is the highest ground in Beechamwell.

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