首页 | 期刊介绍 | 编委会 | 道德声明 | 投稿指南 | 常用下载 | 过刊浏览 | In English
引用本文:刘付程,彭 俊.基于对数比转换方法的沉积物粒级组分空间预测与底质类型制图[J].海洋科学,2015,39(6):122-128.
【打印本页】   【HTML】   【下载PDF全文】   查看/发表评论  下载PDF阅读器  关闭
←前一篇|后一篇→ 过刊浏览    高级检索
本文已被:浏览 1703次   下载 2443 本文二维码信息
码上扫一扫!
分享到: 微信 更多
基于对数比转换方法的沉积物粒级组分空间预测与底质类型制图
刘付程1, 彭 俊2
1.淮海工学院 测绘工程学院;2.盐城师范学院 城市与资源环境学院
摘要:
以废黄河三角洲表层粒度分析数据为基础, 探讨了对数比转换和kriging 插值相结合方法在沉积物粒级组分空间预测和底质类型制图中的应用。结果表明, 基于沉积物粒级组分原始数据的kriging 预测方法难以保证各组分预测结果的非负和定和要求, 因而预测结果的可信度低; 而对数比转换kriging方法不但满足非负和定和要求, 而且还有着更优的组分预测结果和较高的底质类型制图精度。新方法对于开展定量化的沉积物粒级组分预测和底质类型制图具有参考价值。
关键词:  对数比转换  沉积物粒级组分  空间预测  底质制图
DOI:10.11759/hykx20130529001
分类号:
基金项目:国家自然科学基金项目(41306077); 淮海工学院自然科学基金项目(Z2014017)
A logratio transformation based kriging method for spatial prediction of sediment grain size compositions and sediment type mapping
Abstract:
The sediment grain size data are compositional data and are characterized by non-negative and constant sum. In spatial prediction of grain size compositions, one important aspect of the prediction quality is whether the prediction results meet the requirements of non-negative and constant sum, which is also the essential condition for sediment type recognition and mapping. In this paper, the grain size data obtained from the abandoned Yellow River Estuary are taken as an example to discuss the application of combined logratio transform and ordinary kriging in spatial prediction of grain size compositions and sediment type mapping. Results show that the kriging interpolation results by directly using the grain size data are unreliable owing to their dissatisfaction of non-negative and constant sum, while the prediction results obtained using the logratio-transformed grain size data and kriging interpolation method not only meet those two requirements, but also have a better prediction accuracy of grain size compositions and a relative high sediment type mapping precision. So the new method of combined logratio transform and ordinary kriging has reference value for quantitative sediment mapping.
Key words:  logratio transformation  sediment grain size composition  spatial prediction  sediment type mapping
版权所有 《海洋科学》 Copyright©2008 All Rights Reserved
主管单位:中国科学院 主办单位:中国科学院海洋研究所
地址:青岛市市南区福山路32号  邮编:266071  电话:0532-82898755  E-mail:marinesciences@qdio.ac.cn
技术支持:北京勤云科技发展有限公司