首页> 外文期刊>Indian Journal of Geosciences >Study of creek systems of the western Sunderbans with special reference to appraisal of the georesources of the tidal domain
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Study of creek systems of the western Sunderbans with special reference to appraisal of the georesources of the tidal domain

机译:研究西桑德班斯河的小溪系统,特别是对潮汐域的地质资源的评估

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An understanding of the evolution in georesources within the tidal domain could be made through closer appreciation of tidal landforms relating to creek systems. Historically and traditionally, landform units of tidal regime of the Sunderbans have collectively been looked upon as resources for both survival and livelihood. A change in hydraulic regime of the tidal system over last several centuries is manifested in creek systems and hence the quality of the micro-landform units and pattern of their utilisation has witnessed major transformation. With deterioration of discharge along trunk channel of Ganga River, the downstream drainage network and tidal creeks were flushed only with tidal flows. Thus the creek systems, many of which were earlier having sufficient draught for large vessels to ply, had been abandoned and a similar fate followed for some of the ancient habitations. Major changes in land use practices in Sunderbans during British period brought new settlements and the process of building up of land in the intertidal marshes by tide-borne silts carried by creeks was arrested. The creeks further witnessed shallowing of channel beds, changes in configuration of channel bars and tidal flats. The georesources of creeks and associated landforms went through modifications partly due to anthropogenic interference and because of natural instability of the tracts. The study by Geological Survey of India in recent years (2005-2009) indicates that many of the creeks and minor cross channels show rapid deterioration in the north, while outfall points of major creeks show extensive modifications in channel morphology. Various in-channel landforms including channel bed geometry, tidal flats, mid-channel shoals and bars and creek margins have been studied extensively during the survey and their resource potential assessed. As the trend of changes in tidal domain is complex in nature, flexibility in landform- resource utilisation and principle of sequential land use practice should be incorporated in perspective planning of landform-georesources of this fragile domain at land-sea interface. The present study aims at bringing together geological history of the trunk river (Bhagirathi) and the evolution of creek systems of Sunderbans into a broad framework of tidal georesource potential—a step towards this objective.
机译:可以通过更深入地了解与溪流系统有关的潮汐地貌,来了解潮汐域内地质资源的演变。在历史上和传统上,桑德班人的潮汐政权的地形单位被集体视为生存和生计的资源。在小溪系统中,潮汐系统水力状况在过去几个世纪中发生了变化,因此,微地形单位的质量及其利用方式已经发生了重大变化。随着恒河干渠的排放恶化,下游的排水网络和潮汐小溪仅被潮汐冲刷。因此,小河系统已经被抛弃,其中许多早先的吃水深度足以供大型船只使用,因此一些古老的居住区也面临着类似的命运。在英国时期,桑德班人的土地使用方式发生了重大变化,带来了新的定居点,并且由于小溪携带的潮汐淤积物,在潮间带沼泽地中积蓄了土地。小溪还目睹了河床床的变浅,河床横梁和滩涂结构的变化。小河和相关地貌的地质资源经过了部分修改,这是由于人为干扰和土地的自然不稳定性所致。印度近年来(2005-2009年)的地质调查研究表明,许多小河和较小的交叉河道在北部迅速恶化,而主要小河的出水口表明河道形态发生了广泛的变化。在调查期间,对各种河道内地貌进行了广泛研究,包括河床床的几何形状,滩涂,河道中段浅滩和河道以及河道边缘,并对它们的资源潜力进行了评估。由于潮汐域变化的趋势本质上是复杂的,因此应该在陆海界面对这种脆弱域的地貌-地质资源的远景规划中纳入地貌资源利用的灵活性和顺序土地使用实践的原则。本研究旨在将主干河(Bhagirathi)的地质历史和桑德班斯的小溪系统的演变整合到一个广泛的潮汐地质资源潜力框架中,这是朝着这一目标迈出的一步。

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