ISWC OpenIR  > 水保所知识产出(1956---)
贵州省地面组成物质对区域土壤侵蚀的影响
高华端
学位类型博士
导师李锐
2008
学位授予单位中国科学院研究生院
学位授予地点陕西
学位专业土壤学
摘要采用宏观与微观相结合的研究方法,以土壤侵蚀原理为基础,论文研究了贵州省常见地面组成物质对区域土壤侵蚀的影响。结果表明,地面组成物质不仅在微观上影响土壤机械组成,而且在宏观上影响着地表侵蚀地貌的发育及植被类型。同时,地面组成物质与土壤可蚀性及抗冲性方面存在密切的关系。主要研究结论如下:1不同类型地面组成物质发育土壤的砂粒、粉砂粒、黏粒及水稳性团粒均存在显著差异。碳酸盐岩组形成的土壤砂粒含量低(17.84%)而粉砂粒(43.93%)与黏粒(38.24%)含量高,紫色砂页岩与砂页岩土壤均具有砂粒含量高而粉砂粒和黏粒含量较低的特点。碳酸盐岩组发育土壤的以0.52mm水稳性团粒含量最高,砂页岩组发育土壤以0.250.5mm水稳性团粒含量为最高,而板岩组形成的土壤则以大于5mm的水稳性团粒含量最高。在总体水稳性团粒含量方面,板岩组(78.16%)>玄武岩组(65.19%)>碳酸盐岩组(60.68%)>煤系地层(58.96%)>砂页岩组(47.52%)>紫色砂页岩组(42.1%)。2地面组成物质对坡耕地土壤可蚀性K值影响显著。贵州省常见地面组成物质发育土壤具有较强的抗蚀性,可蚀性K值介于0.180.26之间。与滇东北地区土壤相比,结果小得多。3、不同类型地面组成物质发育的坡耕地土壤抗冲性差异显著。其冲刷模数的顺序为:紫色砂页岩组(24.75 g.(m2.s)-1>砂页岩组(21.09g.(m2.s)-1>碳酸盐岩组(14.02g.(m2.s)-1>玄武岩组(10.08g.(m2.s)-1>板岩组(8.78g.(m2.s)-1)>煤系地层(4.89g.( m2.s)-1)。随着水稳性团粒含量的增加,冲刷模数逐渐减小。同时,15mm的水稳性团粒及总水稳性团粒含量与土壤冲刷模数间关系较为密切,且成对数关系。4、地面组成物质对地表侵蚀地貌有显著影响地面组成物质对地表侵蚀地貌的影响表现为不同岩组水道发育状况的差别。水道发育过程在区域上表现出 “随机步行”的普适原则,地面组成物质的差异不影响水道系统内部的自身规律。不同尺度的水道之间,水道级别存在一定的对比和转换关系,1/20万水道系统图所体现的1级水道长度相当于1/5万的23级水道,1/5万水道系统图所体现的1级水道长度相当于1/1万的3级水道。地面组成物质显著地影响着低级水道的数量、总长及平均长,影响相应的水道频度及水道密度,从而造成不同地面组成物质间常态侵蚀的差异。对水道频度的影响次序为:(板岩组,11.88.km-2>(砂页岩组,8.48. km-2;玄武岩组,8.00. km-2;煤系地层,5.98. km-2>(碳酸盐岩组,3.66. km-2)。同时,碳酸盐岩组的面积比例与水道系统间存在较好的相关性。5、贵州省地面组成物质制约着植被类型,显示出非地带性特征。6、建立了基于地面组成物质的贵州省区域土壤侵蚀强度分区及土壤侵蚀危险程度分区。 总之,在贵州省及其类似地区,地面组成物质的多样性控制着区域土壤侵蚀的空间分异规律,是区域土壤侵蚀研究不可忽视的重要因子。研究成果将为区域土壤侵蚀评价、预测预报提供科学依据。
其他摘要Based on the principle of soil erosion, using the research methods combining large scale and small scale, the paper studied the general ground substance’s impact on regional soil erosion in Guizhou Province. Results show that ground substances not only affect soil’s mechanical or physical composition in small scale, but also affect erosion landscape and vegetation in large scale . Meanwhile, there are close relationship between ground substance and soil’s errodibility or anti-scouring. The main research results are as follow.1. There are significant differences among soils developed from different ground substances about sand grain ratio, silt ratio, clay ratio and water-stable aggregation. The soil developed from carbonatite group has lower sand grain ratio (17.84%) but higher silt ratio (43.93%) and higher clay ratio (38.24%). The soils developed from purple sand-shale and sand-shale have higher sand grain ratio and lower clay ratio. About water-stable aggregation, the research indicates that carbonatite’s soil has highest percentage on 0.5-2mm level, sand-shale’s soil has highest percentage on 0.25-0.5mm level and that slate group’s soil has highest percentage on the level over 5mm. On the total water-stable aggregation, there is an order as follow: slate group (78.16%) > basalt group (65.19%) > carbonatite group (60.68%) >coal series (58.96%) > sand-shale group (47.52%) > Purple sand-shale group (42.1%).2. Ground substances significantly affect soil’s errodibility value K on slope cultivated lands. In Guizhou Province, the soils developed from general ground substance have strong anti-errodibilitywhich is between 0.18 and 0.26 and greatly lower than those of northeast area of Yunnan Province. 3. Slope cultivated land soils developed from different ground substances have obviously different anti-scouring ability. The scouring modulus order is as follow: purple sand-shale group (24.75g.(m2.s)-1) > sand-shale group (21.09g.(m2.s)-1) > carbonatite group (14.02g.(m2.s)-1) > basalt group (10.08g.(m2.s)-1) > Slate group (8.78 g.(m2.s)-1) > coal series (4.89g.(m2.s)-1).Soil’s scouring modulus reduces along with increasing of water-stable aggregation content. Meanwhile, there is a close logarithm correlation between water-stable aggregation ratio on 1 to 5mm level and soil’s scouring modulus.4. Ground substance has significant influence on surface erosion landscapeGround substance’s influence on surface erosion landscape is reflected by different water-way’s developing degree on different rock groups. The water-way’s developing process shows a universal law, that is, a random walking principle. The difference of ground substance does not influence a water-way system’s inner laws. Between the different scales, there are certain contrasts or transition relationships for water-way’s levels. Water-way’s length of the first level on water-way system map of 1:200000 scale is amount to the length of the second or third level on 1:50000 scale.  Water-way’s length of the first level on water-way system map of 1:50000 scale is amount to the length of the third level on 1:10000 scale. Ground substances affect lower level water-way’s number, total length, average length, frequency and density, which causes the different normal erosion on different ground substance types. The influence order indicated by water-way’s frequency is as follow:Slate group (11.88 /km2) > sand-shale group (8.48/km2) > basalt group(8.00/km2)> coal series(5.98/km2) >carbonatite group (3.66/km2).Meanwhile, there is a close relationship between the area ratio of carbonatite group and water-way system.5. Ground substances affect the vegetation types and indicate a certain character of non-zonation.6. Establishing the regional division system for soil erosion degree and soil erosion potential danger based on ground substance in Guizhou Province.All in all, in Guizhou Province or similar areas, the diversity of ground substance controls regional soil erosion’s spatial distribution laws. Ground substance is an important factor and shouldn’t be ignored during regional soil erosion studying. Research results will provide the scientific foundation for regional soil erosion’s evaluation and prediction.
文献类型学位论文
条目标识符sbir.nwafu.edu.cn/handle/361005/4077
专题水保所知识产出(1956---)
推荐引用方式
GB/T 7714
高华端. 贵州省地面组成物质对区域土壤侵蚀的影响[D]. 陕西. 中国科学院研究生院,2008.
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
查看访问统计
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[高华端]的文章
百度学术
百度学术中相似的文章
[高华端]的文章
必应学术
必应学术中相似的文章
[高华端]的文章
相关权益政策
暂无数据
收藏/分享
所有评论 (0)
暂无评论
 

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。