Spatial and temporal variations of overland flow during rainfall events and in relation to catchment conditions     

C. M. Orchard  S. A. Lorentz  G. P. W. Jewitt  V. A. M. Chaplot 《水文研究》2013,27(16):2325-2338

Improved knowledge on overland flow (OF) generation and its dynamics (i.e. spatial and temporal variations) is essential to understand catchment hydrology, a prerequisite for better water resources and soil management. In this study, our main objective was to quantify the dynamics of OF during rainfall events and to assess its main factors of control. The research study was undertaken in an agricultural 23‐ha catchment of a communal pasture in KwaZulu‐Natal (South Africa) experiencing Mediterranean climate and with variations of soil, topography and vegetation conditions. The dynamics of OF was evaluated during three rainfall seasons (2007 to 2010) by using 1 × 1‐m² microplots (n = 15) located at five landscape positions. At each location, a microplot was equipped with an automatic tipping bucket linked to a logger to estimate the delay between the start of the rain and the start of OF [i.e. the time to runoff initiation (TRI)]. Multivariate analysis was applied to the total OF and TRI data and the information on selected environmental factors (rainfall characteristics; soil type; soil clay content, Clay; proportion of the soil surface covered by vegetation, Cov; proportion of the soil surface covered by crusting, Crust; mean slope gradient, S; soil bulk density, ρ_b; soil water tension at different depths, SWT). The average OF rate over the 3‐year study period varied 2.3‐fold across the catchment (from 15% footslope to 35% backslope), whereas the average TRI varied by a 10.6‐fold factor (between 0.6 min at bottomland and 6.4 min at footslope). TRI temporal variations correlated the most with event duration (r = 0.8) and cumulative amount of rainfall since the onset of the rainy season (r = ?0.47), whereas TRI spatial variations were controlled the most by Crust (?0.97 < r < ?0.77). Ultimately, TRI spatial variations were modelled and mapped in an attempt to model OF dynamics over the entire microcatchment. Copyright © 2012 John Wiley & Sons, Ltd.  相似文献   

华南海滩剖面沉积物粒度特征影响因子分析     

曹惠美  蔡锋  苏贤泽 《台湾海峡》2010,29(1):73-80

通过对2003年7月采集的华南沿海12条海滩剖面（3种海滩类型）的76个沉积物样品粒度分析，讨论了物质来源、地形地貌、风暴、水动力条件以及后滨向陆的极限高度等对海滩沉积物的性质与分布的影响．研究得出，后滨向陆的极限位置处于相对稳定的状态；后滨的极限高度随着滩面粒径的增大而增加．  相似文献   

Seasonal Variation and Meteorological Control of CO2 Flux in a Hilly Plantation in the Mountain Areas of North China          下载免费PDF全文

HUANG Hui  ZHANG Jinsong  MENG Ping  FU Yuling  ZHENG Ning  GAO Jun 《Acta Meteorologica Sinica》2011,25(2):238-248

The carbon cycle of terrestrial ecosystems is an important scientific issue in global climate change re- search. Plantation forest plays an important role in terrestrial carbon budget in China. In this study, eddy covariance flux data measured at Xiaolangdi forest ecosystem research station (XLD) in 2007 and 2008 are used to analyze the seasonal variation and meteorological control of CO2 flux in a 30-yr-old mixed plantation. The plantation forest mainly consists of Quercus variabilis, Platycladus orientalis, and Robinia pseudoacacia. The results show that the seasonal variations of net ecosystem exchange of CO2 (NEE), gross primary production (GPP), and ecosystem respiration (Re) display single-peak curves. The maximum of carbon sequestration appears during May and June each year. The relative contribution of carbon re- lease from ecosystem respiration to GPP varied slightly between 2007 and 2008. The relationship between NEE and photosynthetic active radiation (Qp) accords with the rectangular hyperbola model on diurnal scale, and shows a good linear correlation on monthly scale. The ecosystem photosynthetic parameters: the maximum photosynthetic rate (Pmax), the ecosystem photosynthetic photonyield (α), and the daytime ecosystem respiration (Rd) exhibit seasonal variations. Pmax reaches the maximum in August each year, with small interannual di?erence. The interannual differences of α and Rd are obvious, which is attributed to the changes of meteorological factors, such as solar radiation, vapor pressure deficit (D), precipitation, etc. Parameters Re, GPP, and NEP (net ecosystem production) have obvious exponential relations with temperature on monthly scale. There is a hysteresis in the response of GPP and NEP to temperature, i.e., the carbon sequestration is not the maximum when the temperature reaches the peak value. The Q10 values were 1.37 and 1.45 in 2007 and 2008, respectively. On monthly scale, Re, GPP, and NEE increase as D increases, but rise slowly and even decrease when D is higher than 1.5 kPa.  相似文献   

Intertidal gastropod assemblages shaped by key environmental variables across the northern Persian Gulf and the Gulf of Omanss     

Fatemeh Amini‐Yekta  Mohammad Reza Shokri  Abdolvahab Maghsoudlou  Hassan Rajabi‐Maham 《Marine Ecology》2019,40(3)

Variations in environmental factors can alter the species distribution pattern in intertidal rocky shores. The Persian Gulf (PG) and the Gulf of Oman (GO) vary substantially with respect to environmental and oceanographic conditions. The abundance and biodiversity of intertidal rocky gastropods in five locations across the northern PG and the GO were compared, and the environmental variables underlying the distribution pattern of these organisms were investigated. A total of 67 gastropod species were identified. The largest average density (294 ind./m²) and diversity (N = 43) for gastropods occurred in the Hotel Lipar station (LIP) located in Chabahar Bay in the GO. Clypeomorus bifasciata (107.43 ind./m²) followed by Cerithium caeruleum (94.67 ind./m²) were the most abundant species. Planaxis sulcatus and Siphonaria spp. occurred in all locations during both sampling occasions. Species richness and abundance of gastropods showed significant differences between LIP and remaining locations. A significant difference was found in assemblage structure across locations. In general, the species richness and density in the locations at GO were significantly larger than those locations in the PG, suggesting that the harsh environmental condition in the PG might be the forcing factor for this diminish. Distinct grouping was observed in both assemblage structure and species composition between locations in the PG and the GO. The spatial and temporal distribution patterns of gastropods assemblages were significantly correlated with variation in salinity and substrate rugosity.  相似文献   

青藏高原西部、南部和东北部边界地区天然水的水化学性质及其成因   总被引：1，自引：1，他引：1  

田原  余成群  查欣洁  高星  于明寨 《地理学报》2019,74(5):975-991

特殊的地理和人文环境致使青藏高原天然水拥有独特的水化学性质并保存着较完整的原生状态,但随着人类活动强度的持续增大,可能导致当地水环境及水化学性质发生改变。通过对青藏高原存在人类活动的西部、南部和东北部边界地区进行水样采集、分析与测定,并探讨了当地天然水水化学性质的区域差异及其成因规律。结果表明：青藏高原不同边界地区天然水的物理性质、水化学性质和成因均存在差异,这些差异主要是地理环境、地质条件等综合作用的结果;水样pH的平均值为7.75,总溶解固体（TDS）的均值为171 mg/L,总硬度（TH）的均值为168 mg/L,总体来看水质较好,大部分能够满足国家和世界卫生组织（WHO）生活饮用水卫生标准,适宜饮用;水样中Ca ²⁺和Mg ²⁺为主要阳离子,HCO₃ ^-和SO₄ ^2-为主要的阴离子,主要由碳酸盐的风化和蒸发岩的溶解共同控制且碳酸盐岩风化的过程更为强烈;各边界地区天然水中的生物源物质均远低于国家和WHO标准,表明目前这些地区受人类活动的影响仍较小。  相似文献   

STUDY ON FLUXES OF CH4 EMISSION FROM PADDY FIELDS IN CHANGCHUN AREA   总被引：1，自引：0，他引：1  

YAN Min hua  MA Xue hui  WANG De xuan 《中国地理科学(英文版)》2000,(3)

CH4 is a kind of important greenhouse gases in atmosphere. The current atmospheric concentration of CH4 is about 1.7ppmv and is increasing at almost 2％ per year. The sources of CH4 include paddies, wetland and tundra, insects, the digestive tracts of ruminants, coal mining, biomass burning, and the leakage of natural gas. The total input to the atmosphere lies in the range 300－ 550Tg per year. CH4 from paddy fields is about 10％ － 20％ of total source of atmospheric CH4 (DING, 1997). …  相似文献   

湖南省县域乡村反贫困绩效评价与空间分异特征   总被引：2，自引：4，他引：2  

谭雪兰  蒋凌霄  米胜渊  欧阳巧玲  王振凯  安悦 《地理科学》2019,39(6):938-946

综合运用熵值法、地理探测器等方法,从基本生存绩效、自身发展绩效,县域扶贫绩效3个方面构建指标体系,对湖南省51个贫困县2017年反贫困绩效空间地域分异特征及其影响因素进行研究。结果表明：① 湖南省贫困农户一般能满足基本的生存需要;自身发展绩效水平得分较高的区域大多处于武陵源区、鹤城区等城市市区周围以及罗霄山片区,而雪峰山脉周围县市则普遍较低;县域扶贫绩效水平高的区域分布较为零散,大致位于各城区周围,而省城或西北的少数民族聚集区以及中南部绩效水平还有待提高。② 反贫困绩效总体上呈现出高、中、低3种绩效水平交替分布的空间特征,愈靠近武陵源区、鹤城区和长株潭地区的贫困县市,综合反贫困绩效水平愈高。③ 县域发展情况是影响湖南省反贫困绩效的决定性因素,农户条件与乡村状况是基础性因素,自然条件是重要因素,各因子间交互作用的影响远大于单因子,不存在独立作用的因素,体现出湖南省反贫困绩效影响因素的复杂性特征。  相似文献   

天气因素对城市地铁客流时空分布的影响——基于智能交通卡数据的实证研究   总被引：1，自引：0，他引：1  

许熳灵  付晓  汤君友  刘志远 《地理科学进展》2020,39(1):45-55

城市地理空间、气候环境及交通系统间存在复杂的相互联系、相互制约的关系,交通及地理时空数据为理解三者间关系带来了新的机遇。城市轨道交通是居民绿色出行、缓解中国大城市交通拥堵的重要交通方式。深入研究影响城市地铁客流时间和空间分布变化的因素,有利于制定合理的土地利用及交通需求管理政策,也可为实时响应特定天气条件下旅客出行需求的变化和优化公交服务运营提供理论依据。论文使用智能交通卡数据,以南京市为例,通过建立一种季节性差分自回归移动平均(seasonal autoregressive integrated moving average with explanatory variables, SARIMAX)模型,解释不同种类的天气因素(如降雨、气温、相对湿度、风速等)对地铁客流量时空分布的影响程度。研究发现：降雨类因素在高峰和周末时段对地铁客流量的影响较大;各天气因素对各地铁站点客流量的影响大致呈现出从城市中心区域向外围区域逐渐变小的渐变式规律,且地铁无规律出行者比有规律出行者更易受恶劣天气因素的影响。  相似文献   

中国三大城市群经济与环境协调度时空特征及影响因素     

张国俊  王珏晗  吴坤津  许志桦 《地理研究》2020,39(2):272-288

采用熵值法、泰尔指数、空间自相关、马尔科夫链等方法,分析2006—2016年中国京津冀、长江三角洲、珠江三角洲三大城市群经济与环境协调度的时空格局特征,并运用Tobit模型探讨其影响因素。结果表明：① 研究期内三大城市群经济与环境协调度持续增长,珠三角协调度最高,长三角协调度增速最快;② 三大城市群内部城市之间的差异波动减小,珠三角城市群的减小幅度最小;③ 三大城市群经济与环境协调等级演化具有一定的路径依赖,但随时间推移有向高一级状态转移趋势;④ 行政级别较高的城市及部分沿海沿江发达城市的经济与环境协调度持续处于较高水平;⑤ 三大城市群经济与环境协调度空间特征由分散走向集聚;⑥ 经济发达的城市经济与环境趋向于“同步发展”;⑦ 能源消耗水平、科学技术水平、固定资产投资强度、外资依存度和所有制结构对三大城市群的经济与环境协调度具有影响,但各因素影响的显著程度有差异。  相似文献   

京津冀地区县域环境胁迫时空格局及驱动因素   总被引：1，自引：0，他引：1  

周侃  李会  申玉铭 《地理学报》2020,75(9):1934-1947

环境胁迫反映人类生产生活过程中污染物输出对区域环境系统产生的综合压力。本文基于县域污染物排放和人口社会经济数据库,运用熵权法综合测度县域环境胁迫指数（ESI）,解析2012—2016年京津冀地区环境胁迫的时空格局及各类主体功能区环境胁迫特征,并针对县域环境胁迫的空间效应,在STIRPAT模型框架基础上,运用地理加权回归方法定量估计县域环境胁迫的社会经济驱动力。结果表明：① 京津冀地区面临的环境胁迫态势显著缓解,2012年以来ESI降幅达到54.68%。其中,以北京、唐山、天津、石家庄等中心城区以及滨海新区下降最为显著,县域环境胁迫程度由中心城区向外围呈梯度递减,到2016年环境胁迫高等级县域已经消除;② 5年间京津冀地区县域环境胁迫的空间溢出效应趋强,并在津唐地区呈现空间锁定和路径依赖;③ 优化开发和重点开发区域两类城市化地区是京津冀水气环境的主要承压区,其环境胁迫程度占京津冀地区全域的65.98%,仍然是环境污染防治与管控的重点区域;④ 人口规模和经济发展水平是县域环境胁迫的控制性因素,此外还受环境处理技术水平、农业生产投入强度、国土开发强度以及城镇化等因素影响;⑤ 各驱动因素对县域环境胁迫的驱动作用存在空间异质性,需针对驱动力作用强度及其空间差异,采取差别化环境治理与源头减排对策,精准提升京津冀地区环境协同管制效果。  相似文献