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Developing Inventory of Riparian Buffer Cover in L'Anguille River Watershed using Geospatial Technologies

机译:利用地理空间技术开发L'Anguille River流域河岸缓冲覆盖的清单

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A watershed level analysis was conducted in East-central Arkansas along L'Anguille River and its major tributaries to assess vegetation composition in riparian buffer cover using two baselines - stream centerline and stream bank. The input data for the study comprised 1:24,000 scale National Hydrography Dataset Plus (NHDPIus) stream centerline, one meter resolution natural color digital ortho quarter quad (DOQQ) imagery, one meter resolution color infrared (CIR) DOQQ imagery, and 2006 land use-land cover (LULC) imagery. Since both the approaches required accurate stream centerline data, manual editing of NHDPIus stream centerline was performed to match streams with their actual locations. The edited stream location was verified by overlaying it on one meter color DOQQ imagery. The first approach was based on identifying the boundary of river/stream banks. The pixels identifying the boundary of river and stream banks were located on natural color and CIR DOQQ imagery by running an automated search in a direction perpendicular to both left and right side of nodal points for each segment of stream centerline. The search algorithm utilized differences in digital number (DN) values for water and land to identify pixels that marked the boundary of landarea immediately adjacent to the water. These identified pixels were joined together to create the boundary of river/stream banks. Adjacent to this boundary of river/stream banks, a 45-m (approx. 148 ft) wide land area, parallel to the banks and consisting of forests and grasslands, was considered "buffer" for mitigating water quality. This approach was compared with previously cited approach in the literature, i.e. buffer creation around stream centerline. The percentage of water pixels present in thevegetation composition analysis performed in buffer area created by using boundary of river/stream banks and stream centerline, respectively, was used as a criteria for measuring the accuracy of both the approaches. The buffer created using boundary of river/stream banks had 27.7% less water pixels compared to stream centerline approach using the natural color imagery. The automated search approach was evaluated for its use on natural and CIR imagery. Several streambank segments were manually delineatedand the error was calculated by measuring the distance between automatic and manual streambank delineations using both imagery types. It was observed that CIR imagery performed better with a mean error of 2.21 m (RMSE 3.07 m) while natural color imageryhad a mean error of 2.55 m (RMSE 3.41 m). Overall, the results show that delineation of boundary of river/stream banks using geospatial techniques and its subsequent use for buffer analysis enhances the accuracy of determining the presence of specifiedsize (width) riparian buffer along river and streams.
机译:流域水平分析是在沿着L'Anguille River的东部 - 中央阿肯色州进行的,主要的支流使用两个基线 - 流中心线和流银行评估河岸缓冲覆盖物中的植被组成。该研究的输入数据包括1:24,000级国家水流数据集加(NHDPIUS)流中心线,一米分辨率自然彩色数字ortho四分之一(Doqq)图像,一米分辨率彩色红外线(CIR)Doqq Imagery,2006年土地使用 - 民居(Lulc)图像。由于这两种方法都需要精确的流中心线数据,因此执行了NHDPIUS流中心线的手动编辑,以将流与实际位置匹配。通过将其覆盖在一米的颜色Doqq图像上来验证编辑的流位置。第一种方法是基于识别河流/流银行的边界。识别河流和流银行的边界的像素位于自然颜色和CIR DOQQ图像上,通过在垂直于小型点中心线的节点左右侧的方向上运行自动搜索。搜索算法利用水和土地的数字数量(DN)值的差异来识别标有水平邻近水的Landarea边界的像素。这些所识别的像素连接在一起以产生河流/流银行的边界。毗邻河流/溪流银行的这个边界,45米(约148英尺)宽的土地面积,与银行平行并由森林和草原组成,被认为是缓解水质的“缓冲区”。将这种方法与先前引用的文献中的方法进行了比较,即河流中心线周围的缓冲区创建。在通过使用河流/流银行和流中心线的边界产生的缓冲区中,在通过使用河流/流银行和流中心线的边界进行的缓冲区中存在的水像素中存在的水像素百分比用作测量方法的准确性的标准。与使用自然彩色图像的流中心线方法相比,使用河流/流银行边界创建的缓冲器具有27.7%的水像素。评估自动搜索方法的自然和CIR图像上的使用。手动描绘了几个StreamBank段和通过使用两种图像类型测量自动和手动流频繁描绘之间的距离来计算错误。观察到CIR图像更好地表现出2.21米(RMSE 3.07 M)的平均误差,而自然颜色Imageryhad为2.55米的平均误差(Rmse 3.41米)。总体而言,结果表明,利用地理空间技术划定了河流/流银行的边界及其随后的缓冲分析的用途增强了确定沿河和流沿河和流沿河流的探测(宽度)河岸缓冲区的存在的准确性。

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