Results 31 to 40 of about 1,125 (146)
Numerical Simulation of Windbreak and Sand Fixation Effects of an Integrated Sand-retaining Dike and Sand-fixing Brick System [PDF]
, 2022 [Objective] In view of the sand burying problem caused by the wind and sand flow on the highway in Bashang area of Zhangjiakou City, Hebei Province, a comprehensive wind and sand fixing system of sand retaining dike sand fixing brick was established, and
Li Jiayuan +5 more
core +1 more source
Computational Simulation of Landform Change in a Fluvial-Aeolian Interacting Field [PDF]
, 2018 传统上对干旱地区地表环境的研究是以风蚀动力为主，然而地球地貌的演化是各种自然过程及环境因子相互作用的结果，风蚀地貌亦然。自20世纪60年代以来，不断有研究人员注意到地球甚至火星地表风蚀沙丘与河流相互影响的现象或痕迹，发现地球地层记录中广泛存在干旱环境的风水交互沉积，从而认识到风水交互作用对地貌的发展与环境变化的联系。但由于风蚀、水蚀地貌的驱动机制不同，风沙地貌与流水地貌的研究是相对独立发展的。因此，研究不同时空尺度下风水交互作用的动力机制、风水交互作用对土壤侵蚀 ...
刘保莉
core
Shuitu Baochi Xuebao, 2003 由风蚀所导致的土壤物质再分配过程,决定了土地沙漠化的程度。根据半干旱干草原地区不同程度沙漠化土地土壤风蚀率的137Cs示踪结果,沙漠化各个阶段的土壤风蚀率指标为:潜在沙漠化土地以微弱堆积和微度风蚀为特征,风蚀率小于2000kg/(hm2·a);轻度沙漠化土地风蚀率介于2000～7000kg/(hm2·a)之间;中度沙漠化土地风蚀率大于7000kg/(hm2·a);重度沙漠化土地风蚀和堆积都很强烈,地表物质交换迅速,没有必要制定风蚀指标。
张春来 邹学勇 董光荣
doaj +2 more sources
萨拉乌苏河流域150 ka BP 以来的粒度旋回 [PDF]
, 2001 萨拉乌苏河流域米浪沟湾地层剖面150 ka BP 以来古流动砂丘砂与河湖相和古土壤在粒度上具有多次显著的粗细韵律交替变化, 粒度参数- M z、R、Sk、Kg 和SC/ D 亦随之响应为多波动峰谷交替的态势。同时, 粒度特征值- 5 5、5 16、5 25、5 50、5 75、5 84、5 95 相应地表现为非常有节奏地跳动。据此, 将米浪沟湾剖面划分为27 个粒度粗细沉积旋回, 并认为其是150 ka BP 以来在东亚冬夏古代季风交替影响下沙漠演变的一个颇为完整的气候- 地质过程记录。The ...
Jin, H +8 more
core
Effect of Freezing on Wind Erosion Resistance of Sand Dune Soil [PDF]
[Objective] To investigate the effect of winter soil freezing on soil erodibility and anti-erodibility in the Yellow River section of the Ulan Buh Desert.
DOU Chunhua +4 more
core +1 more source
Theme-based Second Language Learning through Multimodal Experimental Animation [PDF]
, 2021 In a digital, multimedia, and globalized world, new theories such as multimodality, multiliteracies, and theme-based instruction have signaled a shift in the Chinese as language art and Chinese as second language teaching and learning.
Li, Bailu, Xu, Yuan
core +1 more source
Soil Erosion and Its Spatial Distribution Characteristics in Three-River-Source National Park [PDF]
, 2023 [Objective] The Three-River-Source National Park (TRSNP) is considered to be the “water tower of China”, and is an important ecological security barrier in China.
Huang Tingting +5 more
core +1 more source
Shuitu Baochi Xuebao, 2004 土壤风蚀沙化是北方农牧交错带农牧业生产与发展的主要限制因子,通过室内风洞实验研究,定量分析了土壤风蚀率(风蚀强度)与风速及土壤水分的相关关系、土壤风蚀输沙量的空间分布规律以及翻耕后土壤风蚀的动态变化。结果表明:风蚀率与风速变化成正相关,随着风速增大,风蚀率相应增加,18m/s风速是风蚀由轻变重的一个转折点;土壤水分与风蚀率呈负相关,水分含量越高,风蚀率越小,6%含水量水平是土壤风蚀由重变轻的一个转折点。通过曲线拟合表明,风蚀率与风速成幂函数的关系,与土壤水分含量成对数函数关系 ...
何文清 高旺盛 妥德宝 赵沛义
doaj
Hydrogeological structure of shallow-buried coal seam in wind erosion landform area and water-retaining coal mining method [PDF]
Xinjiang has an arid climate and scarce water resources, thus rendering the protection of water resources a major issue for coal mining. Taking the Yushuquan Coal Mine in Xinjiang as the study area, this study investigated the hydrogeological structure ...
CAI Jin +6 more
core +1 more source
Shuitu Baochi Xuebao, 2006 通过风洞实验，研究了科尔沁沙地两种典型风沙土的风蚀特征。流动沙丘土样和农田土样的风蚀率随风速的增加均呈幂函数关系增长。风干的农田土样在风速3．7m／s时开始出现风蚀现象，但流沙土样的临界起沙风速是4．3m／s。在低风速段．农田土样的风蚀率大于流沙土样，但当风速增加到大约5．7m／s以上时，流沙土样的风蚀率开始大于农田土样，并且差值随风速的增加而加大。两种土样的风蚀率随土样含水率的增加呈负幂函数关系迅速减小。但流沙土样风蚀率的减小要比农田土样更迅速。流沙土样的临界起沙风速随含水量的增加呈线性关系增长 ...
移小勇 +4 more
doaj