scholarly journals FAUNA OF FREELIVING NEMATODES IN THE UKRAINIAN PART OF THE DANUBE RIVER MOUTH AREA IN THE MODERN PERIOD

2020 ◽  
Vol 25 (2(47)) ◽  
pp. 97-112
Author(s):  
І. І. Кулакова
Keyword(s):  
River Mouth ◽  
Mouth Area ◽  
Danube River ◽  
The Danube River ◽  
Modern Period ◽  
River Mouth Area ◽  
Freeliving Nematodes

THE INITIAL RESULTS OF THE SUSPENDED SEDIMENT DYNAMICS DURING THE DRY SEASON IN THE HAU RIVER MOUTH AREA

2017 ◽  
Vol 17 (2) ◽  
Author(s):  
Nguyen Ngoc Tien ◽  
Dinh Van Uu ◽  
Nguyen Tho Sao ◽  
Do Huy Cuong ◽  
Nguyen Trung Thanh ◽  
...  
Keyword(s):  
Suspended Sediment ◽  
River Mouth ◽  
Dry Season ◽  
Sediment Dynamics ◽  
Mouth Area ◽  
River Mouth Area ◽  
Initial Results

Why should the Odra River mouth area not be regarded as an estuary? A geologist's point of view

2007 ◽  
Vol 36 (2) ◽  
Author(s):  
Andrzej Osadczuk ◽  
Stanisław Musielak ◽  
Ryszard Borówka
Keyword(s):  
Coastal Lagoons ◽  
River Mouth ◽  
Mouth Area ◽  
Point Of View ◽  
River Mouth Area ◽  
Open Sea ◽  
Odra River ◽  
Flow Through ◽  
The Baltic ◽  
Shallow Water Body

Why should the Odra River mouth area not be regarded as an estuary? A geologist's point of viewThe authors find no arguments that would justify application of the term "estuary" to the area of the Odra River discharge into the Baltic Sea. The physiography, geology, and hydrology of the Odra river mouth show that the area possesses many more characteristics typical of flow-through coastal lagoons than those of estuaries. Of key importance in this respect is the Szczecin Lagoon, an extensive, shallow water body separated from the open sea by a barrier intersected by three narrow and long straits. The lagoonal nature of the area is demonstrated also by its geological history.

Hydrological and morphological processes at the Zhujiang River mouth area, China

2006 ◽  
Vol 33 (3) ◽  
pp. 237-248 ◽  
Author(s):  
V. N. Mikhailov ◽  
M. V. Mikhailova ◽  
V. N. Korotaev
Keyword(s):  
River Mouth ◽  
Mouth Area ◽  
River Mouth Area ◽  
Morphological Processes ◽  
Zhujiang River

Influence of river discharge and wind field on the freshwater meiofauna of a dynamic river mouth area

2005 ◽  
Vol 163 (3) ◽  
pp. 307-327 ◽  
Author(s):  
A. Witthöft-Mühlmann ◽  
W. Traunspurger ◽  
K. O. Rothhaupt
Keyword(s):  
Wind Field ◽  
River Discharge ◽  
River Mouth ◽  
Mouth Area ◽  
River Mouth Area

scholarly journals Annual layers in river-bed sediment of a stagnant river-mouth area of the Kitagawa Brook, Central Japan

2015 ◽  
Vol 367 ◽  
pp. 251-257
Author(s):  
Y. Kurashige ◽  
T. Nakano ◽  
E. Kasubuchi ◽  
M. Maruo ◽  
H. Domitsu
Keyword(s):  
River Mouth ◽  
Mouth Area ◽  
Contaminated Water ◽  
Deciduous Trees ◽  
Bed Sediment ◽  
Central Japan ◽  
River Mouth Area ◽  
River Bed ◽  
Sand And Gravel ◽  
River Bed Sediment

Abstract. The river mouth of Kitagawa Brook is normally stagnant because it is easily closed by sand and gravel transported by littoral currents of Biwa Lake, Japan. A new urban area exists in the basin and sewerage works were constructed in the early 1990s, so contaminated water with a bad odour had flowed into the brook before the sewerage works. To reduce the smell, the river mouth was excavated to narrow the channel in the early 1980s. Thus, river-bed sediment after this excavation only occurs at the river mouth. From the upper 24 cm of a sediment core, we found 19 strata of leaves which were supplied from deciduous trees in autumn. We also found several gravel layers which were supplied from the lake during severe storms. The combination of veins and gravel layers were reconstructed for about 20 years of sediment records with an error of two to three years.

scholarly journals MAJUNYA GARIS PANTAI YANG DIAKIBATKAN OLEH PROSES SEDIMENTASI DI SEPANJANG PANTAI PERAIRAN KABUPATEN REMBANG

2016 ◽  
Vol 6 (3) ◽  
Author(s):  
Deny Setiady ◽  
Ediar Usman
Keyword(s):  
Coastal Area ◽  
Sandy Beach ◽  
River Mouth ◽  
Mouth Area ◽  
Sediment Supply ◽  
Coastal Morphology ◽  
River Mouth Area ◽  
Sea Bottom ◽  
Sandy Coast ◽  
Very High

Majunya garis pantai yang terjadi di sekitar pantai perairan Rembang melingkupi daerah yang luas. Kondisi ini disebabkan morfologi pantai yang sangat landai dan pasokan sedimen yang tinggi terutama di sekitar muara sungai Pasokan sedimen dari sungai yang mengalir ke pantai utara Rembang membentuk endapan sedimen permukaan dasar laut. Sedimen tersebut juga menimbulkan akrasi sepanjang pantai Berdasarkan pemetaan karakteristik pantai perairan Rembang terdiri dari pantai berpasir, pantai berlumpur, pantai berbatu dan terumbu. Akrasi terjadi pada pantai berpasir dan terumbu. Kata Kunci: Majunya garis pantai, Sedimen, Rembang The emerging land in Rembang coastal area is very widely distributed. This is due to a very flat coastal morphology and very high sedimentary supply especially found around river mouth area. Sediment supply from rivers mouthed to north Rembang coast form sea bottom surficial sediment. The sediment is also causing emerging land or accretion along the coastal area of Rembang. Based on coastal characteristics mapping Rembang coastal area consisted of sandy coast, muddy coast, rocky beach and reefy coast. Accretion occurred at sandy beach and reefy coast Keyword: Emerged Land, Sediment, Rembang

Water level fluctuations in the Odra River mouth area in relation to passages of deep low-pressure systems

2007 ◽  
Vol 36 (1) ◽  
Author(s):  
Bernard Wiśniewski ◽  
Halina Kowalewska-Kalkowska
Keyword(s):  
Sea Level ◽  
Atmospheric Pressure ◽  
River Mouth ◽  
Storm Surges ◽  
Low Pressure ◽  
Mouth Area ◽  
Water Level Fluctuations ◽  
River Mouth Area ◽  
Odra River ◽  
Low Pressure Systems

Water level fluctuations in the Odra River mouth area in relation to passages of deep low-pressure systemsThe Odra River mouth area is affected by storm surges caused by passages of deep low-pressure systems over the Baltic Sea. The surges are the result of wind action and changes in atmospheric pressure at the sea surface. The two effects may be additive, in which both factors increase or decrease the sea level on the coast, or they may be non-additive, where one factor increases the sea level and the other decreases it. This paper discusses the role of the wind field and changes in atmospheric pressure in the duration and extent of storm surges in the Odra River mouth area.

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