东北低山丘陵典型区侵蚀沟分布特征及其地形影响研究     

焦鹏  阎百兴  欧洋  李明堂  任明  温磊磊  崔虎  田莉萍  程磊  刘惠平 《地理科学》2022,42(10):1829-1837

东北低山丘陵区是重要的粮食主产区和商品粮基地,高强度的农业垦殖造成了严重的水土流失,侵蚀沟危害日益加剧。选择东辽河上游106.5 km²的区域为研究区,基于分辨率2 m的遥感影像,在GIS人工预判读侵蚀沟的基础上,野外实地验证并测量了研究区内长度≥50 m、且深度≥0.5 m的侵蚀沟的几何参数与经纬度;基于DEM获取了侵蚀沟所在坡面的坡度、坡向和高程等空间信息;分析了研究区侵蚀沟的基本特征与时空演化趋势,探讨了坡度和坡向对侵蚀沟发育的影响。结果表明：① 目前研究区已形成侵蚀沟322条,分布密度为3.0条/km²,沟壑密度为0.8 km/km²,割裂度为1.4%,侵蚀沟发展速度快,沟蚀强度已达强烈程度,应引起足够重视。② 侵蚀沟主要分布在6°~9°的坡耕地上,坡度对沟蚀的影响明显,坡耕地高强度垦殖是沟蚀加剧的主要驱动力;③ 阳坡（S、E）上侵蚀沟分布相对较多,而阴坡（N）上侵蚀沟分布最少,坡向对沟蚀也有一定影响。研究成果为认识东北低山丘陵区侵蚀沟发生与演化提供了科学数据。  相似文献   

中亚五国自华进口贸易技术溢出及碳排放影响研究          下载免费PDF全文

黄丽  王武林  龚姣 《干旱区地理》2022,45(3):986-997

梳理1992—2018年中亚五国碳排放变化过程,运用碳排放库兹涅茨曲线模拟人均碳排放与人均国内生产总值（GDP）的关系,基于中亚五国人均GDP、工业增加值、研发投入、自华进口中间品和资本品的技术溢出存量等指标,构建面板数据固定效应模型以探究碳排放影响机制。结果表明：（1） 中亚五国碳排放先降后升,各国碳排放的变化率波动较大,其中哈萨克斯坦碳排放占中亚五国碳排放比重最大。（2） 就人均碳排放与人均GDP拟合的碳排放库兹涅茨曲线关系而言,哈萨克斯坦和土库曼斯坦表现为倒N型,乌兹别克斯坦、塔吉克斯坦、吉尔吉斯斯坦和中亚五国表现为N型。（3） 中亚五国自华进口额呈现较快的增长趋势,其中自华进口的中间品和资本品合计约占自华进口总额的3.920%~10.976%,中亚五国整体及各国中间品技术溢出存量均明显大于资本品技术溢出存量。（4） 在影响中亚五国碳排放的诸多因素中,人均GDP和工业增加值占GDP比重的回归系数显著为正,人均GDP、工业增加值占GDP比重每上升1%,碳排放分别增加0.337%和0.343%,研发投入、交互项LnZJ_it×LnS_it（中间品技术溢出存量的自然对数×工业增加值占GDP比重的自然对数）的回归系数显著为负,研发投入每增加1%,碳排放可减少约0.432%,在降低因工业增加值占GDP比重上升导致的碳排放方面,中间品技术溢出存量的影响极小。  相似文献   

Simulation of the Subsidence and Deposition Processes of the Foreland Basin in the Southwestern Margin of Ordos     

Liu Shaofeng  Li Sitian  Zhuang Xinguo  Jiao Yangquan  Lu ZongshengChina University of Geosciences  Wuhan 《《地质学报》英文版》1996,70(3):233-245

Characteristics of deformation in the thrust belt and sequence stratigraphic framework in the foreland basin, structural features of the basin margin, and the episodic thrusting are studied in this paper by combining the eastern Qilian thrust belt and the Late Triassic foreland basin on the southwestern margin of Ordos. On this basis, a geological model and a mechanical model of coupling mechanism were established for the pair of thrust belt and foreland basin, and the subsidence and deposition process of the foreland basin were simulated on given parameters.  相似文献   

南极威德尔-斯科舍汇流区上层湍流混合特征及其与水团和环流的联系     

林丽金  史久新  姚辰阳  郭桂军  程灵巧  矫玉田  施骞 《极地研究》2022,34(1):34-50

利用中国第32次南极科学考察队于2015年12月至2016年1月在南极威德尔-斯科舍汇流区获得的湍流微结构、温盐深仪和下放式声学多普勒海流计观测资料,分析了该海域上层海洋(30～500 dbar)的湍流混合空间分布特征.结果显示,湍动能耗散率(ε)和湍扩散系数(Kρ)分布呈现明显的区域性特征,与当地的水团和环流分布密切...  相似文献   

雅满苏地区中酸性岩浆岩同位素年代学特征及意义     

黎娇  王高  刘祥  王哲  凤骏 《中国地质调查》2022,9(1):54-63

雅满苏地区跨越多个区域构造带,过往研究对于每个构造带的形成、相对构造运动形式、相对构造运动规模存在较大争议.通过采集不同构造带内中酸性岩体的岩石样品,对雅满苏地区3个构造带内的中酸性岩体开展岩石学、地球化学以及锆石U-Pb同位素年代学研究.结果表明:除苦水混杂岩带花岗斑岩(TW-1)为过铝质钙碱性I型花岗岩,其他2个构...  相似文献   

内蒙古银额盆地查干凹陷构造-层序-沉积特征、盆地原型及其成因机制^*          下载免费PDF全文

杨国臣  焦大庆  肖斌  陈明权  刘建军  王彦丽 《古地理学报》2013,15(3):305-316

通过对钻井、测井、三维和二维地震资料的综合研究,将内蒙古银额盆地查干凹陷白垩系至新生界划分为2个一级层序、4个构造层序、6个超层序和11个层序。根据等时层序格架下各层序单元内部的沉积充填演化特征,建立了不同级次构造成因层序的构造-层序关系。在此基础上,结合构造应力机制研究和区域构造应力场演化,采用平衡剖面技术解析查干凹陷的构造-沉积史,将该凹陷的构造和沉积演化序列划分为4个一级构造-沉积演化阶段和若干二级、三级构造-沉积演化阶段,进而分析了各构造-沉积演化阶段的构造和沉积特征、凹陷原型的性质及成因机制。  相似文献   

A distributed runoff model for the mountainous region of the Heihe River Basin (China) based on the spatial modeling environment (SME) I: model structure and equations     

Wenxian Jiao  Zhongmin Xu 《Environmental Earth Sciences》2013,68(3):881-888

A shortage of water has limited the socio-economic development of the Heihe River Basin in northwestern China and has led to many ecological and economic problems. Only the development and application of integration tools can effectively represent the functionality of the watershed and aid in strategic decision making. In the framework of SME, modular and hierarchical model building can simplify the research work. According to the main ideas and key processes commonly used in distributed hydrological models, and combined with the spatial characteristics of the mountainous region of the Heihe River Basin, a unit hydrological model was developed using stella, which was an icon-based software package specifically designed for dynamic systems modeling, and an algorithm for spatial distribution in SME was introduced. This paper describes only the model structure and basic equations, whereas in the next paper, model calibration results using the data measured at meteorological stations, together with land use data and soil data, will be further introduced.  相似文献   

Using stable isotopes of surface water and groundwater to quantify moisture sources across the Yellow River source region     

Xingxing Kuang  Xin Luo  Jiu Jimmy Jiao  Sihai Liang  Xiaolang Zhang  Hailong Li  Junguo Liu 《水文研究》2019,33(13):1835-1850

Characterization of stable isotope compositions (δ²H and δ¹⁸O) of surface water and groundwater in a catchment is critical for refining moisture sources and establishing modern isotope–elevation relationships for paleoelevation reconstructions. There is no consensus on the moisture sources of precipitation in the Yellow River source region during summer season. This study presents δ²H and δ¹⁸O data from 111 water samples collected from tributaries, mainstream, lakes, and groundwater across the Yellow River source region during summertime. Measured δ¹⁸O values of the tributaries range from ?13.5‰ to ?5.8‰ with an average of ?11.0‰. Measured δ¹⁸O values of the groundwater samples range from ?12.7‰ to ?10.5‰ with an average of ?11.9‰. The δ¹⁸O data of tributary waters display a northward increase of 1.66‰ per degree latitude. The δ¹⁸O data and d‐excess values imply that moisture sources of the Yellow River source region during summertime are mainly from the mixing of the Indian Summer Monsoon and the Westerlies, local water recycling, and subcloud evaporation. Analysis of tributary δ¹⁸O data from the Yellow River source region and streamwater and precipitation δ¹⁸O data from its surrounding areas leads to a best‐fit second‐order polynomial relationship between δ¹⁸O and elevation over a 4,600 m elevation range. A δ¹⁸O elevation gradient of ?1.6‰/km is also established using these data, and the gradient is in consistence with the δ¹⁸O elevation gradient of north and eastern plateau. Such relationships can be used for paleoelevation reconstructions in the Yellow River source region.  相似文献   

FORMATION MECHANISM AND SPATIAL PATTERN OF URBAN AGGLOMERATION IN CENTRAL JILIN OF CHINA     

QIN Gan ZHANG Ping-yu JIAO Bin 《中国地理科学(英文版)》2006,16(2):154-159

1 INTRODUCTION Urban agglomeration researches originated from the concern about the city cluster in the developed areas of western countries. The modern researches have been extended to the specific areas. HALL (2001) summa- rized the generality and difference of urban metropoli- tans in Europe, and analyzed the spatial structure of dif- ferent areas. NAUDE and KRUGELL (2003) analyzed the spatial development of urban agglomeration in South Africa, and thought that the size of the p…  相似文献   

夏日哈木超大型镍矿I号岩体地幔源区性质和硫化物熔离过程：来自橄榄石成分、亲铜元素和硫同位素的约束     

李中州  王亚磊  王梦玺  焦建刚  夏明哲 《地质学报》2023,97(10):3326-3346

夏日哈木超大型镍矿I号岩体的地幔源区目前仍存在软流圈、大陆下岩石圈地幔和辉石岩地幔三种不同认识。本次研究通过对该岩体西段新近发现的隐伏矿体ZK3109钻孔中斜方辉石岩和浸染状矿石中的橄榄石进行原位成分分析,识别地幔源区性质,并结合硫化物原位S同位素和全岩亲铜元素组成,探讨硫化物熔离过程。样品中橄榄石均具有较低的Mn/Zn比值(基本小于13.5),而且斜方辉石岩中橄榄石具有较低的100×Mn/Fe比值(基本小于1.35),指示岩体源区有辉石岩地幔组分加入,与前人根据硫化物矿体富Ni特征的推测一致。橄榄石低Ca(小于300.00×10^-6)、高Li(平均9.83×10^-6)以及Sc与Ni正相关指示辉石岩地幔组分可能是俯冲洋壳物质交代大陆下岩石圈地幔的产物。另一方面,斜方辉石岩中橄榄石Ni、Fo值均与Co负相关且全岩S和铂族元素(PGE)相关性不明显,说明浅部岩浆房硫化物熔离发生在斜方辉石岩形成之后。浸染状矿石中橄榄石Co和Ni正相关且全岩S和PGE正相关,暗示橄榄石成分受控于硫化物熔离。样品中镍黄铁矿、磁黄铁矿和黄铜矿δ³⁴...  相似文献