黑龙江省耕地时空变化及驱动因素分析   总被引：3，自引：0，他引：3  

李丹  周嘉  战大庆 《地理科学》2021,41(7):1266-1275

以黑龙江省1980年、1990年、2000年、2010年、2015年5期土地利用数据为基础,综合利用GIS手段和地理探测器模型,确定1980—2015年4个时期黑龙江省耕地变化的时空分异特征及主要驱动因素。研究结果表明,1980—2015年黑龙江省耕地数量总体增加,增加的耕地主要来源于林地、草地和未利用地。各时期耕地数量变化具有明显差异,以1990—2000年耕地数量变化最多。各时期耕地变化空间差异特征明显。1980—2015年黑龙江省耕地利用动态度呈现出先升高后降低的趋势,耕地利用动态度活跃区域集中在三江平原和松嫩平原地区。各时期驱动因子的解释能力不同,人口数量、政策因素、GDP以及城镇化水平是解释能力较强的驱动力因子。驱动因子对耕地时空变化的影响是通过各个因子之间的交互作用实现的,表现为双因子增强和非线性增强。  相似文献   

高考试题中地理时间思维的解析     

牛超 《地理教学》2021,(1):8-13

地理时间思维是主观思维对客观地理事象时间存在及其特征的反映。依照地理事象历时变化与共时关联的存在形式,地理时间思维分为历时思维与共时思维。地理时间思维具有动态性、关联性、尺度性、预见性与时效性的特征。本文基于地理时间思维的基本内涵与特征表现,解析了近年高考文科综合能力测试(地理)全国卷中蕴含的时间思维及其特征的体现,意在通过地理时间思维的视野,对地理现象与地理问题形成不同层面的认识,促进与深化对地理“综合思维”的理解。  相似文献   

电竞产业空间格局演化及其影响因素     

詹绍文  朱一鑫  程哲  窦世斌 《热带地理》2021,41(2):303-314

基于上海市2006—2018年电竞企业的数据,综合运用核密度估计、最邻近指数、Kriging空间插值分析等方法,探讨上海市电竞产业的空间演化过程及影响因素。结果表明：1）电竞产业可以划分为2006—2010年的起步阶段,2010—2014年的快速发展阶段,2014—2018年的爆发增长阶段;2）电竞产业在空间分布上由双核心聚集发展为多核心聚集,具有整体上中心聚集、同时向外扩展的特征,南北方向是企业扩展的主要方向;3）高资本电竞企业主要向软件园区和高等院校聚集,呈现出4个高资本热区,这些热区未来更有机会出现更具竞争力的电子竞技企业;4）政府政策规划对电竞产业的区位选择具有导向作用,高质量人力资源、经济发展水平、周边电竞市场环境、交通便捷性是企业聚集的基础力量;与传统产业相比,由于电子竞技产业具有体育性的竞技特征,其竞技水平和赛事举办也会对产业发展产生重大影响。  相似文献   

Relationship between sand-dust weather and water dynamics of desert areas in the middle reaches of Heihe River     

Yun Niu  XianDe Liu  Xin Li  YanQiang Wei  Hu Zhang  XiaoYan Li 《寒旱区科学》2016,8(6):516-523

Sand-dust weather has become an international social-environmental issue of common concern, and constitutes a serious threat to human lives and economic development. In order to explore the responses of natural desert sand and dust to the dynamics of water in desertification, we extracted long-term monitoring data related to precipitation, soil water, groundwater, and sand-dust weather. These data originated from the test stations for desertification control in desert areas of the middle reaches of the Heihe River. We used an algorithm of characteristic parameters, correlations, and multiple regression analysis to establish a regression model for the duration of sand-dust weather. The response characteristics of the natural desert sand and dust and changes of the water inter-annual and annual variance were also examined. Our results showed: (1) From 2006 to 2014 the frequency, duration, and volatility trends of sand-dust weather obviously increased, but the change amplitudes of precipitation, soil water, and groundwater level grew smaller. (2) In the vegetative growth seasons from March to November, the annual variance rates of the soil moisture content in each of four studied layers of soil samples were similar, and the changes in the frequency and duration of sand-dust weather were similar. (3) Our new regression equation for the duration of sand-dust weather passed the R test, F test, and t test. By this regression model we could predict the duration of sand-dust weather with an accuracy of 42.9%. This study can thus provide technological support and reference data for water resource management and research regarding sand-dust weather mechanisms.  相似文献   

南沙红树林湿地公园水环境质量时空差异分析——基于改进后倍斜率聚类分析的视角     

宋焱  徐颂军  刘贤赵  张勇  邱鹏华  牛安逸  许观嫦 《地理科学》2016,36(2):303-311

于2007年和2014年的丰水期和枯水期分别测量了南沙红树林湿地公园一期、二期及其附近河涌8个采样点的水体温度、pH、DO、COD、BOD₅、TP和TN等物化指标。通过对比监测结果和倍斜率聚类评价结果发现：研究区水质总体上处于Ⅱ级-Ⅲ级或Ⅱ级-Ⅳ级的“尚清洁”状态;红树林湿地公园一期2008年对外开放后至2014年,水环境指标中pH变化范围不大,DO、COD含量有所下降,BOD₅、TP和TN含量均呈增加趋势;2007年南沙红树林湿地公园一期采样点W1、W2、W3水质优于河涌采样点W7和W8,河涌采样点W7和W8水质优于红树林湿地公园二期采样点W4、W5、W6;2014年南沙红树林湿地公园二期采样点W4、W5、W6水质优于红树林湿地公园一期采样点W1、W2、W3和河涌采样点W7、W8;8个采样点中水质改善最明显的是二期采样点W6,水质下降最明显的是一期采样点W3;丰水期河涌水质2014年较2007年有所好转,但红树林湿地公园水质无论枯水期亦或丰水期,多数情况下优于河涌水质;研究区域水环境质量的时空差异总规律为2007~2014年南沙红树林湿地公园二期水质好转,一期水质有所下降。  相似文献   

Environmental quality and sources of heavy metals in the topsoil based on multivariate statistical analyses: a case study in Laiwu City,Shandong Province,China   总被引：1，自引：0，他引：1  

Lei Yu  Jiemin Cheng  Jincheng Zhan  Aixia Jiang 《Natural Hazards》2016,81(3):1435-1445

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基于改进NCC算法的东南极极记录冰川流速提取研究          下载免费PDF全文

牛牧野周春霞  刘婷婷 《极地研究》2016,28(2):243-249

南极冰川的流速在南极物质平衡研究中有着重要的作用。将SIFT算子的旋转参数引入传统的基于归一化互相关(NCC)的冰川流速提取方法,使其拥有旋转不变的特性。利用此方法,基于Landsat 8 OLI数据对东南极的极记录冰川流速进行了提取,并通过利用模拟影像和NASA发布的MEa SUREs冰川流速结果对该方法的精度进行了验证。结果表明,改进的NCC算法能够在冰川流速方向改变区域提取更多的流速信息,极记录冰川流速最大可达870m·a~(-1),提取结果与MEa SUREs结果相比,平均偏差为23.9 m·a~(-1)。  相似文献   

The subducted oceanic crust within continental-type UHP metamorphic belt in the North Qaidam, NW China: Evidence from petrology, geochemistry and geochronology   总被引：25，自引：0，他引：25  

Guibin Zhang  Shuguang Song  Lifei Zhang  Yaoling Niu 《Lithos》2008,104(1-4):99-118

Three types of eclogite, together with a serpentinized harzburgite, coexist as blocks within granitic and pelitic gneisses along the Shaliuhe cross section, the eastern part of the North Qaidam continental-type ultrahigh-pressure (UHP) metamorphic belt, NW China. The olivine (Ol¹) and orthopyroxene in the harzburgite are compositionally similar to present-day abyssal peridotites. The kyanite–eclogite is derived from a troctolitic protolith, whereas the epidote–eclogite from a gabbroic protolith, both having distinct positive Eu anomalies, low TiO₂, and high Al₂O₃ and MgO. The kyanite–eclogite shows inherited cumulate layering. The phengite–eclogite has high TiO₂, low Al₂O₃ and MgO with incompatible trace elements resembling enriched-type MORB. Sr–Nd isotope data indicate that the protoliths of both kyanite–eclogite and epidote–eclogite ([⁸⁷Sr/⁸⁶Sr]_i ~ 0.703–0.704; ε_Nd(T) ~ 5.9–8.0) are of mantle origin (e.g., ocean crust signatures). On the other hand, while the lower ε_Nd(T) value (1.4–4.1) of phengite–eclogite is more or less consistent with an enriched MORB protolith, their high [⁸⁷Sr/⁸⁶Sr]_i ratio (0.705–0.716) points to an additional enrichment in their history, probably in an subduction-zone environment. Field relations and geochemical analyses suggest that the serpentinized harzburgite and the three types of eclogite constitute the oceanic lithological section of an ophiolitic sequence from mantle peridotite, to cumulate, and to upper basaltic rocks. The presence of coesite pseudomorphs and quartz exsolution in omphacite plus thermobarometric calculations suggests that the eclogites have undergone ultrahigh pressure metamorphism (i.e., peak P ≥ 2.7 GPa). The harzburgite may also have experienced the same metamorphism, but the lack of garnet suggests that the pressure conditions of ≤ 3.0 GPa. Zircon U–Pb SHRIMP dating shows that the eclogites have a protolith age of 516 ± 8 Ma and a metamorphic age of 445 ± 7 Ma. These data indicate the presence of a Paleo-Qilian Ocean between Qaidam and Qilian blocks before the early Ordovician. The ophiolitic assemblage may be the relics of subducted oceanic crust prior to the subduction of continental materials during Ordovician–Silurian times and ultimate continent collision. These rocks, altogether, record a complete history of ocean crust subduction, to continental subduction, and to continental collision.  相似文献   

福建省煤田地质工作回顾     

石礼炎  王振民  詹一振  黄耀明 《福建地质》2008,27(2):94-104

从福建省50多年来承担煤田勘查的队伍演化、煤田地质勘查发展历程、五大煤炭基地勘查简介、煤田地质勘查及研究主要成果等方面进行回顾,总结了福建煤田地质勘查的基本经验和体会,对今后煤田地质工作提出了相关的建议。  相似文献   

钻井液流变模型的优选     

童红梅  乌效鸣  钮洪亮 《岩土钻凿工程》2008,(5):1-4

选择合适的工程浆液流变模型是现场生产中很重要的技术问题。基于最小二乘法原理利用Visual C＋＋高级语言编制程序对试验数据进行拟合,可求得实测浆液的常用流变参数值,绘制各常用流变模式与实际流型的曲线,从而优选出最合适的流变模式。  相似文献