Effects of sand-fixing and windbreak forests on wind flow: a synthesis of results from field experim

来源 :Journal of Arid Land | 被引量 : 0次 | 上传用户:sdn20907
下载到本地 , 更方便阅读
声明 : 本文档内容版权归属内容提供方 , 如果您对本文有版权争议 , 可与客服联系进行内容授权或下架
论文部分内容阅读
Sand-fixing and windbreak forests are widely used to protect or/and improve the ecological environments in arid and semi-arid regions. A full understanding of wind flow characteristics is essential to arranging the patterns of these protective forests for enhancing the effectiveness. In this study, the wind velocity over the underlying surface with sand-fixing forests and windbreak forests at the heights of 1–49 m was monitored from two 50-m high observation towers in an oasis of Minqin, Gansu Province of China. The wind velocities were simulated at different locations over these protective forests between those two towers by a two-dimensional Computational Fluid Dynamics(CFD) model. The results showed that at the heights of 1–49 m, the wind velocity profiles followed a classical logarithm law at the edge of the oasis and a multilayer structure inside the oasis. With increasing number of sand-fixing forest and windbreak forest arrays, the wind velocity at the heights of 1–49 m generally decreased along the downstream direction of the prevailing wind. Specifically, below the height of windbreak forests, the wind velocity decelerates as the airflow approaches to the windbreak forests and then accelerates as the airflow passes over the windbreak forests. In contrast, above the height of windbreak forests, the wind velocity accelerates as the airflow approaches to the windbreak forests and then generally decelerates as the airflow passes over the windbreak forests. Both the array number and array spacing of sand-fixing and windbreak forests could influence the wind velocity. The wind protection effects of sand-fixing forests were closely related to the array spacing of windbreak forests and increased with the addition of sand-fixing forests when the array of the forests was adequately spaced. However, if the array spacing of windbreak forests was smaller than seven times of the heights of windbreak forests, the effects were reduced or completely masked by the effects of windbreak forests. The results could offer theoretical guidelines on how to systematically arrange the patterns of sand-fixing and windbreak forests for preventing wind erosion in the most convenient and the cheapest ways. Sand-fixing and windbreak forests are widely used to protect or / and improve the ecological environments in arid and semi-arid regions. A full understanding of wind flow characteristics is essential to arranging the patterns of these protective forests for enhancing the effectiveness. study, the wind velocity over the underlying surface with sand-fixing forests and windbreak forests at the heights of 1-49 m was monitored from two 50-m high observation towers in an oasis of Minqin, Gansu Province of China. The wind velocities were simulated at different locations over these sheath forests between those two towers by a two-dimensional Computational Fluid Dynamics (CFD) model. The results showed that at the heights of 1-49 m, the wind velocity profiles followed a classical logarithm law at the edge of the oasis and a multilayer structure inside the oasis. With increasing number of sand-fixing forest and windbreak forest arrays, the wind velocity at the heights of 1-49 m ge这个 风速 decelerates as the airflow approaches to the windbreak forests and then accelerates as a airflow direction over the windbreak forests. In contrast, above the height of the windbreak forests, the wind velocity accelerates as the airflow approaches to the windbreak forests and then generally decelerates as a airflow passes over the windbreak forests. both the array number and array spacing of sand-fixing and windbreak forests could influence the wind velocity. wind protection effects of sand-fixing forests were closely related to the array spacing of windbreak forests and increased with the addition of sand-fixing forests when the array of the forests was adequately spaced. However, if the array spacing of windbreak forests was smaller than seven times of the heights of windbreak forests, the effects were reduced or completely masked by the effe cts ofwindbreak forests. The results could offer theoretical guidelines on how to systematically arrange the patterns of sand-fixing and windbreak forests for preventing wind erosion in the most convenient and the cheapest ways.
其他文献
HUANG An finally set footin Hainan, the onlyChinese province he hasnever been to, at the end ofJune. If he had gone in May theprice of his ticket would have be
铜鼓岭位于海南岛文昌县东部海滨,南北长约6公里,东西宽约2公里,它拔地而起,雄奇挺秀,景色迷人,是一个理想的旅游胜地。登上铜鼓岭主峰向东远眺,极目南海,只见水天一色,浩瀚
从四川省成都市乘汽车出发,溯岷江经过灌县的都江堰、茂汶县的迭溪地震湖、千年古城松潘,翻越岷江与嘉陵江的分水岭—贡杠岭,顺嘉陵江水系的白河行程约2小时便到达了我国新
2016年9月26日,四川省社会科学院隆重召开“马克思主义学院成立会议暨邓小平与中国梦学术研讨会”。中共四川省委宣传部李酌副部长出席开幕式并作重要讲话,四川省社会科学院
2017年3月28日,由中国人民大学人文社会科学学术成果评价研究中心、中国人民大学书报资料中心联合研制的“2016年度复印报刊资料转载指数排名”发布。“复印报刊资料转载指数
“到苏州不游虎丘者,乃憾事也。”苏学士这话很对。虎丘是姑苏第一名胜,焉能不去。剑池、白莲池和“天下第三泉”之间,有巨石一片,平坦如砥,高下如削,气势雄伟,人称千人石。
IN the north of Yunnan’s Dali and to the south of ancient Lijiang City lies a basin surrounded by green hills. This basin, called “Bazi,” is bisected by a l
哲学社会科学是一个总称,除了包含最基本的哲学学科外,还包含许多其他相关学科,涵盖历史、政治、经济、文化、社会、生态、军事等各领域,囊括传统学科、新兴学科、前沿学科、
江苏昆山县城玉峰镇北望,在茫茫无际的太湖平原上,耸立着一座巍巍山峰,它就是名闻海内的玉峰山。远观,一峰独秀,峰峦雄峙,巨石嶙峋;近览,灵巧剔透,谐趣柔和,历来被人誉为“
峨眉山的“双桥清音” 是由两条山溪——黑龙江和白龙江汇于清音阁牛心亭前;两江之水冲击在汇合处的巨石——牛心石上,发出清亮深沉的响声回荡在林涧深谷而得名. 如此佳景是