Titlebook: Southern Iraq‘s Marshes; Their Environment an Laith A. Jawad Book 2021 Springer Nature Switzerland AG 2021 Iraqi marshes.Iraqi Wetlands.Mes

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Introduction,he Central Marshes and (iii) Al Hawizeh Marshes. These three chief marsh zones have been at the centre of the great fluctuations that have been in process over the years. Marsh inhabitants who experienced a mixture of pastoralist, inactive and marsh existence grounded on the periodic growth, and col

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Physical and Chemical Characters of Mesopotamian Marshes: A Short Review less than that of the Shatt al-Arab River, whereas silicate value has been varied slightly between 7.7 and 9.8?mg SiO./l. A clear seasonal variation was evident in southern marshes before draining. Water character after reflooding showed slight value of suspended matter, pH value was 6.6–8, and EC

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Hydrologic Structures in the Tigris-Euphrates Basin and Their Impact on the Vitality of the Marshesing alone has not restored the hydrology of the marshlands; instead, further comprehensive data on water discharge and quality is still needed. A management plan would have to find suitable alternative water supplies, especially with regard to discharge which is of low quality, or establish suitable

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Use of Multispectral and Hyperspectral Satellite Imagery for Monitoring Waterbodies and Wetlandsoposed a framework for hyperspectral CD methods on wetland and water body areas. The proposed method is based on incorporating chronochrome, Z-score analysis, Otsu algorithm, SImplex via Split Augmented Lagrangian (SISAL), Harsanyi–Farrand–Chang (HFC), Pearson correlation coefficient (PCC), and supp

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Sedimentology and Mineralogy of Quaternary Sediments of Marshes, South of Iraqcentage of the sand fraction is small in the marshes sediments, but to some extent, it shows a change in heavy and light minerals. The proportion of light minerals is large compared to the proportion of heavy minerals. Light minerals include carbonate, quartz, feldspar, and chert and the heavy miner

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Phytoplankton and Primary Production in Iraqi Marshesant followed by Cyanophyta, Chlorophyta, Cryptophyceae, Pyrrophyceae, and Euglenophyceae. Generally, there are two peaks of phytoplankton bloom that have been recorded: one in autumn and the other in June–July. Chlorophyll . concentration had shown different values at different stations; generally i