华北土石山区,rocky mountain area of northern China
1)rocky mountain area of northern China华北土石山区
1.By studying on the soil water of pine forests and bare soil of shady slope,and Platycladus orientalis and oak mixed forests of sunny slope inrocky mountain area of northern China,there was less illumination time and intensity in the shady slope than in the sunny slope,so the evaporation of shady slope was little,which was propitious to hold water and increase water in the soil.通过对华北土石山区阴坡油松林、阴坡裸地和阳坡侧柏栎类混交林土壤水分研究可知,阴坡光照时间和强度较阳坡小,相应的林地蒸发散减少,有利于林地的蓄水,增加土壤的含水量。
英文短句/例句
1.Soil Health Assessment of the Main Plant Communities in Rocky Mountain Area of North China;华北土石山区典型植物群落土壤健康评价
2.Ecosystem health assessment of the Pinus tabulaeformis forest in earch-rocky mountain area of North China华北土石山区油松林生态系统健康评价
3.Health Analysis and Evaluation of the Main Forest Types in the Typical Soil-gravel Area in North China;华北土石山区典型区域主要类型森林健康分析与评价
4.Basic Study on Directional Adjustment and Control for Stable Protective Forest System Structure in Mountain and Stony Area of North China;华北土石山区防护林体系稳定林分结构定向调控基础研究
5.Study on the Rules of Water Consumption of Dominant Tree Species and the Community of Artificial Forest in Mountain Area of Northern China;华北土石山区典型人工林优势树种及群落耗水规律研究
6.Study on Forest Health Based on Forest Vegetation Succession in Mountain Area of Northern China;华北土石山区基于森林植被演替规律的森林健康的研究
7.The Application of Distributed Hydrologic Model MIKESHE to Simulate Hydrologic Responses of Small Watershed in North China;应用分布式流域水文模型MIKESHE研究华北土石山区小流域水文响应
8.Study on the Ecologuical Response of Hydrology on Forest Vegetation in Some Typical Watershed in North China;华北土石山区典型流域森林植被水文生态过程响应研究
9.The Coupling Relationship between Forest Vegetation and Terrain of Watershed in Earth-rocky Mountainous Area in North China华北土石山区流域森林植被与地形因素耦合关系研究
10.Response of Land Use Change to Hydrological Dynamics in Rocky Mountain Area of North China--Based on Yunzhou Reservoir of Zhangjiakou华北土石山区土地利用/土地覆被变化的水文响应研究——以张家口云州水库流域为例
11.Soil Respiration in Typical Forest Plantations in Lithoid Hilly Areas of North-China;华北石质山区典型人工林土壤呼吸特征的研究
12.Studies on Flora and Ecology of Sacicolous Mosses in Beishan, Jinhua, Zhejiang Province;浙江金华北山石生藓类植物区系和生态学研究
13.Analysis on Transpiration and Difference between Evapotranspiration and Precipitation of Apricot Trees in the Rocky Mountain Area of Northern China华北石质山区杏树蒸腾规律和蒸降差分析
14.Soil Properties Modified with Different Fertilization and Moisture Conservation in the Typical Soil-gravel Area in PingShan County, Hebei Province, China不同施肥保墒材料对河北平山土石山区土壤性状改良的研究
15.Study on Seed-base Method for Afforestation in Saline Land in Hebei and Rocky Mountainous Area in Beijing河北滨海盐碱地和北京土石山区基盘法造林技术研究
16.Evaluation of Indirect Benefits From Rural Development and Debris Flow Prevention Plans-Case of Huashan Area;农村建设与土石流防治计划之间接效益评估——以华山地区为例
17.Changes and Mechanism of Soil Respiration on Winter Wheat Field in Low Mountain and Hill Regions of North China华北低山丘陵区冬小麦田土壤呼吸变化规律及其影响机制
18.Analysis of Soil Organic Carbon Density in the Lithoid Mountainous Area in North China:A Case Study in Miyun County北方石质山区表层土壤有机碳密度特征分析——以密云县为例
相关短句/例句
lithoid mountainous areas in North China华北石质山区
1.Plot-scale runoff generation model oflithoid mountainous areas in North China;华北石质山区坡地产流模型
3)earth-rock mountainous area北方土石山区
1.The study is an attempt to explore the comprehensive eco-economic management model of soil and water conservation in theearth-rock mountainous areas of Northern China.结果表明,通过对流域进行水土保持生态经济型综合模式治理,将流域治理,区域特色,市场推动有机结合起来,不仅使区域生态环境得到了进一步改善,水土流失得到了有效控制,而且带动了区域经济发展,为我国北方土石山区水土保持生态经济型综合治理模式探索提供了技术支持。
4)mountainous area of North China华北山区
1.Themountainous area of North China is surrounded by the North China Plain, Shanxi Gansu Loess Plateau and Inner Mongolia Plateau.华北山区位于华北平原与陕甘黄土高原以及内蒙古高原之间，是我国经济欠发达地区之一。
2.Rainfall simulation on representative plots(5 m wide and 10 m long) in amountainous area of North China was carried out to compare water discharge and recession characteristics by surface runoff,soil-layer flow and mantle rock flow.通过位于北京市怀柔区东台沟的华北山区典型坡面径流场内人工模拟降雨实验,分别讨论了地表径流、壤中流和基岩风化带出流共3层的退水特征,三者比较结果表明,壤中流最早开始退水,其退水历时最长,流量最小;地表径流的退水一般受降雨和地形地貌的影响,雨停后迅速消退;基岩风化带出流通常在地表径流退水的后半段开始。
5)earth-rock mountain region土石山区
6)Tangshan earthquake region华北唐山震区
延伸阅读
华北野战军(见华北军区)华北野战军(见华北军区)North China Field ArmyHuabei Yezhanlun华北野战军(North ehina Field Army)见华北军区。
