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Morphology and channel characteristics of an equatorial tropical river in Malaysian Borneo: a detailed evaluation through spatially explicit geomorphometric modelling

机译:马来西亚北欧赤道热带河流的形态和渠道特征:通过空间明确地形地形造型进行详细评估

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Abstract Geomorphic and morphodynamic characteristics of Akah River in Sarawak, Malaysia in north-western Borneo were modelled using geographical information system assisted techniques and geomorphometric indices. Stream properties such as longitudinal profile, stream length gradient index (SL), channel slope, hypsometric curve, hypsometric integral, sinuosity index and channel cross profiles were analyzed. Morphological features such as meander and channel bar characteristics were evaluated and compared to classify the river and to identify the processes responsible for its present nature. The longitudinal profile, SL index and channel slope indicate the presence of multiple knick points in the channel, which may be indicative of changes in the base level characteristics of the river or lithological differences. The characteristic convex shape of hypsometric toe indicates late stage of deposition due to diffusive processes and the hypsometric integral identifies the geomorphic evolution as in the advanced stage i.e. erosion is?significant. The sinuosity index classifies the entire river as meandering and some segments as tortuously meandering with varied stream valleys. Numerous channel bars of various dimensions are found in different reaches of the stream indicating varying channel bottom characteristics and flow mechanism due to the influence of geological process. The information generated from spatial modelling of different geomorphic indices (different terrain variables) and channel characteristics classifies the Akah subwatershed with slope (diffusive) and fluvial dominated geomorphic process having highly meandering channel and showing anomalous characteristics in some segments. These findings will serve as baseline information, while considering the region for hydrological development activities which include check dams, mini hydroelectric projects.
机译:摘要西北北京萨拉瓦克阿卡河的地貌和形势特征,采用地理信息系统辅助技术和地产镜指数进行了建模。分析了纵向轮廓,流长度梯度索引(SL),通道斜率,低测量曲线,低测量积分,索度指数和通道交叉轮廓等流性质。评估曲折和沟道条特征等形态学特征,并比较河流,并识别负责其本质的过程。纵向轮廓,SL指数和通道斜率表示通道中存在多个knick点,这可以指示河流或岩性差异的基础级别特征的变化。低沉趾的特征凸形形状表明由于扩散过程而沉积的后期,低色积分识别在高级阶段中的几何演变。侵蚀是侵蚀的影响。陷阱指数将整个河流分类为蜿蜒的曲线和一些曲折,与各种流谷的曲折蜿蜒曲折。在物流的不同距离中发现了许多各种尺寸的通道杆,其指示由于地质过程的影响而导致的不同通道底部特性和流动机制。不同地貌指数的空间建模(不同地形变量)和沟道特性产生的信息将具有高曲折通道的斜率(扩散)和河流主导地貌工艺分类为具有高曲折通道的液晶主导地貌工艺,并在一些区段中显示出异常特性。这些调查结果将作为基线信息,同时考虑到水文开发活动的区域,包括检查水坝,迷你水力发电项目。

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