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991.
The run‐off volume altered by the construction of hydropower plants affects ecohydrological processes in catchments. Although the impacts of large hydropower plants have been well documented in the literature, few studies have been conducted on the impacts of small cascaded hydropower plants (SCHPs). To evaluate the impacts of SCHPs on river flow, we chose a representative basin affected by hydropower projects and, to a lesser degree, by other human activities, that is, the Qiuxiang River basin in Southern China. The observed river discharge and climate data during the period of 1958–2016 were investigated. The datasets were divided into a low‐impact period and a high‐impact period based on the number of SCHPs and the capacities of the reservoirs. The daily river discharge alteration was assessed by applying the Indicators of Hydrologic Alteration. To separate the impact of the SCHPs on the local river discharge from that of climate‐related precipitation, the back‐propagation neural network was used to simulate the monthly average river discharge process. An abnormal result was found: Unlike large reservoirs in large watersheds, the SCHPs regulated the flows during the flood season but were not able to mitigate the droughts during the dry season due to their limited storage and the commonly occurring inappropriate interregulations of the SCHPs. The SCHPs also reduced the annual average river discharge in the research basin. The contribution of the SCHPs to the river discharge changes was 85.37%, much higher than the contributions of climate change (13.43%) and other human activities (1.20%). The results demonstrated that the impacts of the SCHPs were different from those of large dams and reservoirs that regulate floods and relieve droughts. It is necessary to raise the awareness of the impacts of these river barriers.  相似文献   
992.
为了研究碱湖N2O释放速率及其对盐度与pH的响应,选取内蒙古大克泊碱湖的五个沉积物样点,采用15N同位素标记模拟实验,研究反硝化和厌氧氨氧化的速率、相对比例和气体产生情况,揭示高盐和高pH对碱湖氮移除的影响。发现大克泊湖潜在氮移除速率为0~16.06 n mol N mL-1 h-1,潜在反硝化速率为0~12.62 n mol N mL-1 h-1,潜在厌氧氨氧化速率为0~9.81 n mol N mL-1 h-1;当盐度34.00 g·L-1与pH 10.22时,厌氧氨氧化对氮移除贡献较大,达到43.18%~71.79%。反硝化过程气体产物以N2为主,几乎无N2O气体释出。另外,该区域潜在氮移除速率与pH呈正相关关系,与TOC、NO-3、HCO-3呈负相关关系;未发现氮移除速率与盐度之间的相关关系。因此,在研究的碱湖中,氮移除过程中主要为N2排放,而N2O低于检测水平;氮移除过程的影响因素复杂且不限于最主要的环境变量(盐度与pH)。这些结果为研究湖泊N2O排放提供了数据基础。  相似文献   
993.
Cheng  Zhiheng  Pan  Hui  Zou  Quanle  Li  Zhenhua  Chen  Liang  Cao  Jialin  Zhang  Kun  Cui  Yongguo 《Natural Resources Research》2021,30(2):1481-1493

With increasing demands for coal resources, coal has been gradually mined in deep coal seams. Due to high gas content, pressure and in situ stress, deep coal seams show great risks of coal and gas outburst. Protective coal seam mining, as a safe and effective method for gas control, has been widely used in major coal-producing countries in the world. However, at present, the relevant problems, such as gas seepage characteristics and optimization of gas drainage borehole layout in protective coal seam mining have been rarely studied. Firstly, by combining with formulas for measuring and testing permeability of coal and rock mass in different stress regimes and failure modes in the laboratory, this study investigated stress–seepage coupling laws by using built-in language Fish of numerical simulation software FLAC3D. In addition, this research analyzed distribution characteristics of permeability in a protected coal seam in the process of protective coal seam mining. Secondly, the protected coal seam was divided into a zone with initial permeability, a zone with decreasing permeability, and permeability increasing zones 1 and 2 according to the changes of permeability. In these zones, permeability rises the most in the permeability increasing zone 2. Moreover, by taking Shaqu Coal Mine, Shanxi Province, China as an example, layout of gas drainage boreholes in the protected coal seam was optimized based on the above permeability-based zoning. Finally, numerical simulation and field application showed that gas drainage volume and concentration rise significantly after optimizing borehole layout. Therefore, when gas is drained through boreholes crossing coal seams during the protective coal seam mining in other coal mines, optimization of borehole layout in Shaqu Coal Mine has certain reference values.

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994.
Zhao  Kang  Zhou  Yun  Yu  Xiang  Yan  Yajing  Song  Yufeng  Wang  Junqiang  Suo  Tianyuan  Guo  Xiao 《Natural Resources Research》2021,30(5):3839-3852
Natural Resources Research - Depletion of shallow mineral resources caused by deep mining has become an inevitable trend, and deep mining can increase safety accidents and geological hazards....  相似文献   
995.
Wang  Zhenzhi  Fu  Xuehai  Deng  Ze  Pan  Jienan 《Natural Resources Research》2021,30(5):3717-3734
Natural Resources Research - In this study, the adsorption–desorption/induced strains/permeability characteristics of seven columnar coal samples with Ro.ran ranging from 0.42 to 3.23% were...  相似文献   
996.
Yin  Xin  Liu  Quansheng  Pan  Yucong  Huang  Xing  Wu  Jian  Wang  Xinyu 《Natural Resources Research》2021,30(2):1795-1815

Rockburst is a common dynamic geological hazard, severely restricting the development and utilization of underground space and resources. As the depth of excavation and mining increases, rockburst tends to occur frequently. Hence, it is necessary to carry out a study on rockburst prediction. Due to the nonlinear relationship between rockburst and its influencing factors, artificial intelligence was introduced. However, the collected data were typically imbalanced. Single algorithms trained by such data have low recognition for minority classes. In order to handle the problem, this paper employed stacking technique of ensemble learning to establish rockburst prediction models. In total, 246 sets of data were collected. In the preprocessing stage, three data mining techniques including principal component analysis, local outlier factor and expectation maximization algorithm were used for dimension reduction, outlier detection and outlier substitution, respectively. Then, the pre-processed data were split into a training set (75%) and a test set (25%) with stratified sampling. Based on the four classical single intelligent algorithms, namely k-nearest neighbors (KNN), support vector machine (SVM), deep neural network (DNN) and recurrent neural network (RNN), four ensemble models (KNN–RNN, SVM–RNN, DNN–RNN and KNN–SVM–DNN–RNN) were built by stacking technique of ensemble learning. The prediction performance of eight models was evaluated, and the differences between single models and ensemble models were analyzed. Additionally, a sensitivity analysis was conducted, revealing the importance of input variables on the models. Finally, the impact of class imbalance on the prediction accuracy and fitting effect of models was quantitatively discussed. The results showed that stacking technique of ensemble learning provides a new and promising way for rockburst prediction, which exhibits unique advantages especially when using imbalanced data.

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997.
边界区类型划分与经济发展水平密切相关,对省际边界区经济协调发展具有参考价值.该文以苏鲁豫皖省际边界区为研究对象,利用空间自相关分析、产业差异度等方法,分析该地区经济发展的时空特征,并从产业结构视角划分边界区类型和边界线类型.主要结论如下:1)苏鲁豫皖省际边界区经济集聚特征明显且不断增强,并出现地域分化现象,各省域内县域经济发展水平差异不断减小,而省域间经济差异在扩大;2)经济发展水平高值区和低值区集聚趋势明显,省际边界效应带来的经济差异呈现显著的地域特征;3)根据省际边界两侧相邻地区的产业结构差异,将边界区划分为"桥梁型"和"切变型",将省际边界线划分为"桥梁型""切变型"和"中间型".  相似文献   
998.
文章选取了学校地理课堂中若干具有代表性的教师提问案例,以学生是否可以较好地表述答案为依据,分析了教师课堂提问的误区,且分别对课堂提问的误区提出了相应的纠正对策,以期帮助教师在课堂中准确提问。  相似文献   
999.
大河流域的水系统是支撑社会-生态系统的基础,理解水系统的结构变化是深入揭示区域系统演化的关键。基于自然-社会水系统视角,从黄河全流域和二级水资源分区尺度,利用1998—2018年降水、蒸发、径流、社会经济耗水等水系统变量,通过Mann-Kendall趋势检验和线性回归分析方法,分析了水系统要素的变化趋势及结构演变特征。结果表明:在全流域尺度,降水、蒸发分别以4.25 mm·a-1、4.09 mm·a-1的速率上升,但蒸发在空间上的变化更显著;径流量呈现先减少再上升后急剧下降的趋势,且与降水量显著正相关。社会系统耗水量呈现增速减缓的特征,农业灌溉占耗水结构的比例以0.50%的速率逐年下降;城镇公共、居民生活和生态环境耗水比例分别以0.07%、0.29%、0.11%的速率上升。在二级水资源分区尺度,各水系统分异特征明显,兰州至头道拐段及花园口以下区域水系统所支撑社会经济发展的功能已经出现了超载。各水系统要素间具有不同程度的协同演变趋势,在湿润区域,蒸发相较于降水具有明显的滞后现象,但在干旱区域两者变化趋势基本一致。黄河流域水系统要素在时空上均存在明显的异质性,未来人口和经济的进一步发展可能会使区域的水资源压力加剧。  相似文献   
1000.
沙丘粒度特征不仅能反映沙丘沙物质的来源与动力,也可以体现地形对风沙流运移的改变。对西藏朋曲流域不同地貌部位流动沙丘表层沉积物的粒度特征进行分析。结果表明:(1)朋曲流域流动沙丘表层沉积物粒度组分以中沙(46.51%)和细沙(40.52%)为主,粗沙(5.87%)与极细沙(5.87%)次之,黏土(0.37%)与粉沙(0.85%)含量最低。流动沙丘表层沉积物平均粒径1.41—2.32 Φ,分选系数0.45—0.79 Φ,偏度0.01—0.24,峰度0.98—1.80。(2)从河漫滩到河流阶地到山坡,流动沙丘粒度逐渐变小,频率分布曲线逐渐变高变窄,粒径越来越集中,沿主导风向自西南向东北概率累积曲线斜率逐渐增大,分选性逐渐变好。(3)河漫滩至河流高级阶地流动沙丘表层沉积物随海拔升高粒径变小,坡麓至坡顶随海拔升高粒径变大,分选却变好,表明山坡上沙丘与阶地上沙丘的沙物质来自于不同河段的河床或河漫滩。  相似文献   
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