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黄河三角洲滩地土壤颗粒分形特征及其与土壤有机质的关系 被引量:57
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作者 吕圣桥 高鹏 +2 位作者 耿广坡 张杰 夏江宝 《水土保持学报》 CSCD 北大核心 2011年第6期134-138,共5页
土壤粒径分布影响土壤的水力特性、土壤肥力以及土壤侵蚀状况等,是重要土壤物理性状之一。以黄河三角洲滩地土壤为研究对象,利用单重与多重分形学理论和方法,对黄河三角洲滩地不同土地利用方式土壤的分形特征及其与土壤有机质的相关性... 土壤粒径分布影响土壤的水力特性、土壤肥力以及土壤侵蚀状况等,是重要土壤物理性状之一。以黄河三角洲滩地土壤为研究对象,利用单重与多重分形学理论和方法,对黄河三角洲滩地不同土地利用方式土壤的分形特征及其与土壤有机质的相关性进行研究。结果表明,不同土地利用方式对土壤单重分形维数D有显著影响,D值介于2.465 7~2.678 9,其中,林地的D值最大,粘粒含量最高,砂粒含量最低;而荒草地的D值最小,粘粒含量最低,砂粒含量最高;土壤粒径分布的多重分形参数D0(容量维数)、D1(信息维数)和D1/D0(信息维数/容量维数)的值因土地利用方式不同而出现规律性的趋势,均表现为刺槐林地>欧美杨林地>棉花地>荒草地;土壤单重分形和多重分形参数均与土壤有机质含量之间存在显著的相关性,而且普遍高于土壤质地与有机质的相关性。土壤分形及多重分形参数能较好地表征黄河三角洲滩地不同土地利用方式对土壤结构性状和土壤肥力的影响与改变,可为黄河三角洲滩地的治理与开发提供理论依据和技术指导。 展开更多
关键词 土壤粒径分布 土地利用方式 多重分形 黄河三角洲滩地
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Dynamics Characteristics and Topographic Profile Shaping Process of Feiyan Shoal at the Yellow River Delta 被引量:1
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作者 应铭 李九发 +1 位作者 陈沈良 戴志军 《Marine Science Bulletin》 CAS 2008年第2期74-88,共15页
Feiyan Shoal is a sub Yellow River Delta, which was formed from Jan. 1964 to May 1976, when the Yellow River entered sea via Diaokou Channel. Since the terminal reach shifted to Qingshuigou channel in 1976, Feiyan Sho... Feiyan Shoal is a sub Yellow River Delta, which was formed from Jan. 1964 to May 1976, when the Yellow River entered sea via Diaokou Channel. Since the terminal reach shifted to Qingshuigou channel in 1976, Feiyan Shoal has been experiencing severe erosion and retreat. This paper explains the evolutionary characteristics of the typical profile of Feiyan Shoal from the perspective of dynamical force and sediments' characteristics. All this is on the basis of the data of topographic profiles observed since the 1970s and the samples of hydrology and sediments collected in situ in Apr. 2004, the analysis of the retreating distance, and the tidal and wave friction velocity distribution. Feiyan Shoal topographical profile has experienced a course of "fast erosion and retrogression - slow eroding modulation - fluctuate triggering change" in recent 30 years, which is also the gradual disappearing process of the delta front. The different intensity of sediment erosion resistance is the main reason for the erosion speed changes. Due to the hydrodynamic force changes, the water depth range of maximum retreating distance and between erosion and progradation became shallow. It indicates that the storm tide will still be the triggering force of seashore topographic profile evolutions in the future. 展开更多
关键词 The Yellow River Delta Feiyan Shoal EROSION wave and tidal co-action topographic profile sediment transport
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