The natural flow regime organizes and defines river ecosystems. In riv translation - The natural flow regime organizes and defines river ecosystems. In riv Malay how to say

The natural flow regime organizes a

The natural flow regime organizes and defines river ecosystems. In rivers, the physical structure of the environment and, thus, of the habitat is defined largely by physical processes, especially the movement of water and sediment within the channel and between the channel and floodplain. The physical habitat of a river includes sediment size and heterogeneity, channel and floodplain morphology, and other geomorphic features. These features form as the available sediment, woody debris, and other transportable materials are moved and deposited by flow. Thus, habitat conditions associated with channels and floodplains vary among rivers in accordance with both flow characteristics and the type and the availability of transportable materials. Within a river, different habitat features are created and maintained by a wide range of flows (Poff et al. 1997).
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Rejim aliran semula jadi menganjurkan dan ekosistem mentakrifkan sungai. Di sungai, struktur fizikal alam sekitar dan, dengan itu, habitat ditakrifkan terutamanya oleh proses fizikal, terutama pergerakan air dan sedimen dalam saluran ini, antara saluran dan dataran banjir. Habitat fizikal sungai termasuk saiz sedimen dan kepelbagaian, Saluran dan morfologi dataran banjir, dan ciri-ciri geomorphic lain. Ciri-ciri ini membentuk sebagai sedimen ada, serpihan kayu, dan bahan-bahan diangkut lain dipindahkan dan disimpan oleh aliran. Oleh itu, keadaan habitat yang berkaitan dengan saluran dan dataran banjir berbeza-beza antara sungai-sungai mengikut kedua-dua ciri-ciri aliran dan jenis dan ketersediaan bahan diangkut. Dalam sungai, ciri-ciri habitat yang berbeza yang dicipta dan disenggarakan oleh pelbagai aliran (Poff et al.
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Rejim aliran semulajadi menganjurkan dan mentakrifkan ekosistem sungai. Di sungai-sungai, struktur fizikal alam sekitar dan, oleh itu, habitat yang ditakrifkan sebahagian besarnya disebabkan oleh proses fizikal, terutamanya pergerakan air dan mendapan di dalam saluran dan di antara saluran dan Dataran. Habitat fizikal Sungai termasuk saiz endapan dan heterogeneity, saluran dan geomorfologi yang biasa, dan ciri lain yang lain. Ini merupakan bentuk yang boleh dijadikan sebagai keladak, Woody serpihan, dan lain-lain bahan yang diangkut dipindahkan dan didepositkan oleh aliran. Oleh itu, keadaan habitat yang berkaitan dengan saluran dan Dataran yang berbeza-beza antara Sungai mengikut kedua-dua ciri aliran dan jenis bahan Meja pengangkutan. Di dalam sungai, ciri habitat yang berbeza dicipta dan diselenggara oleh pelbagai jenis aliran (Poff et Al. 1997). ...
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