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黄土丘陵沟壑区土壤水分垂直变异及影响因素 被引量:16
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作者 邱德勋 赵佰礼 +2 位作者 尹殿胜 穆兴民 高鹏 《中国水土保持科学》 CSCD 北大核心 2021年第3期72-80,共9页
以陕西安塞纸坊沟小流域为例,通过测定0~1000 cm深度土壤含水量,分析不同坡度、坡向和土地利用方式下的土壤水分垂直变异特征。结果表明:1)不同土地利用方式下土壤水分垂直分布特征不同。乔木林地与灌木林地土壤含水量均在0~50 cm减小,... 以陕西安塞纸坊沟小流域为例,通过测定0~1000 cm深度土壤含水量,分析不同坡度、坡向和土地利用方式下的土壤水分垂直变异特征。结果表明:1)不同土地利用方式下土壤水分垂直分布特征不同。乔木林地与灌木林地土壤含水量均在0~50 cm减小,而在50 cm以下乔木林地小幅波动,灌木林地缓慢增大。撂荒草地与农地土壤含水量逐渐升高,最后趋于稳定。2)乔木林地和灌木林地随退耕年限的增加,土壤水分减少,而撂荒草地差异不明显。3)浅层(0~200 cm)土壤含水量:撂荒草地(10.20%)>农地(10.04%)>灌木林地(9.39%)>乔木林地(8.91%);深层(200~1000 cm)土壤含水量:农地(13.50%)>撂荒草地(13.34%)>灌木林地(11.66%)>乔木林地(7.87%)。表明撂荒草地能够较好地保持土壤水分,乔木林地则相对较差。4)坡度对撂荒草地浅层和乔木林地深层土壤水分有显著影响,土壤含水量随坡度增大而减小。坡向对乔木林地和撂荒草地浅层土壤水分有极显著影响,且阴坡土壤水分大于阳坡。总体上,土地利用方式、坡度及其交互作用对浅层土壤水分有显著影响,坡度的贡献率最大(34.85%),土地利用方式对深层土壤水分有显著影响,贡献率为23.03%。地形是浅层土壤水分变异的重要影响因素,而深层土壤水分则主要受土地利用方式的影响。 展开更多
关键词 土壤水分 垂直变异 地形因子 土地利用 黄土丘陵沟壑区
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渭河流域极端降雨变化趋势及其对水沙情势的影响 被引量:7
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作者 邱德勋 穆兴民 +1 位作者 赵广举 高鹏 《水土保持研究》 CSCD 北大核心 2022年第6期65-72,共8页
为探究渭河流域极端降雨变化趋势及其对水沙情势的影响,采用非参数趋势检验、突变检验和连续小波变换诊断了渭河流域1960—2019年的极端降雨指数及径流输沙序列的变异特征,通过双累积曲线法和相关分析法定量评估了流域极端降雨对水沙变... 为探究渭河流域极端降雨变化趋势及其对水沙情势的影响,采用非参数趋势检验、突变检验和连续小波变换诊断了渭河流域1960—2019年的极端降雨指数及径流输沙序列的变异特征,通过双累积曲线法和相关分析法定量评估了流域极端降雨对水沙变化的影响。结果表明:各极端降雨指数呈阶段性波动变化,总体上PRCPTOT,RX5day和RX1day呈不显著下降趋势,R95pTOT,SDII和FSPTOT呈不显著上升趋势。各极端降雨指数均存在以4~6 a,11~12 a,28~29 a为周期的变化特征。径流与输沙量均呈显著减少趋势,分别在1993年、1999年发生突变,其中径流存在5 a和12 a的周期。各极端降雨指数均与径流、输沙量正相关,相比之下,输沙量与各极端降雨指数之间的相关系数偏低。极端降雨变化对径流与输沙量的减少具有重要影响。其中,PRCPTOT对径流减少的影响最大(29.65%),其次是RX5day(25.68%)和FSPTOT(25.95%)。PRCPTOT对输沙量减少的影响也是最大的(10.02%),其次是RX5day(7.12%)。综上,渭河流域水沙情势的变化受极端降雨的显著影响。 展开更多
关键词 渭河流域 水沙 极端降雨
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关中平原极端降水时空变化及其与大气环流的关系 被引量:6
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作者 丁莹莹 邱德勋 +2 位作者 吴常雪 穆兴民 高鹏 《干旱区研究》 CSCD 北大核心 2022年第1期104-112,共9页
基于关中平原13个气象站1957—2019年逐日降水资料,运用一元线性回归、Pearson相关分析和小波相干分析等方法,计算各极端降水指数,分析其时空变化特征,探讨极端降水与大气环流的关系。结果表明:(1)在时间上,除极端降水强度以0.007 mm... 基于关中平原13个气象站1957—2019年逐日降水资料,运用一元线性回归、Pearson相关分析和小波相干分析等方法,计算各极端降水指数,分析其时空变化特征,探讨极端降水与大气环流的关系。结果表明:(1)在时间上,除极端降水强度以0.007 mm·d^(-1)·(10a)^(-1)速率的上升外,其他极端降水指数均呈下降趋势,其中年均极端降水总量(PRCPTOT)下降最快,下降速率为-5.528 mm·(10a)^(-1),并且各极端降水指数均无显著突变点。(2)在空间上,极端降水指数南高北低,空间差异显著。(3)反映大气环流的南方涛动指数(SOI)对极端降水影响最为显著。SOI越大,关中平原越易出现少雨现象。本研究可为关中平原洪水灾害防治提供科学理论依据。 展开更多
关键词 关中平原 极端降水 时空变化 大气环流
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大理河流域干旱变化特征及其与极端降水的关系 被引量:6
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作者 邱德勋 穆兴民 +1 位作者 尹殿胜 高鹏 《干旱区地理》 CSCD 北大核心 2021年第5期1240-1249,共10页
基于标准化降水指数(SPI)方法,对1971—2017年大理河流域干旱变化特征及其与极端降水的联系进行了分析。结果表明:(1)不同时间尺度SPI对降水量变化的敏感程度不同,SPI1和SPI3适用于短期气象旱涝特征的识别,而SPI6和SPI12对揭示区域长期... 基于标准化降水指数(SPI)方法,对1971—2017年大理河流域干旱变化特征及其与极端降水的联系进行了分析。结果表明:(1)不同时间尺度SPI对降水量变化的敏感程度不同,SPI1和SPI3适用于短期气象旱涝特征的识别,而SPI6和SPI12对揭示区域长期旱涝影响及持续时间效果较好。2种时间尺度SPI(SPI3和SPI12)的时间变异性均呈显著增加趋势。(2)不同季节SPI的变化趋势和干旱等级频次存在差异,仅冬季有一定的下降趋势,其余季节呈增加趋势,秋季最显著。年SPI波动幅度较大,总体上呈增加趋势,2001年以来最明显。干旱等级均以轻旱和中旱为主(21.2%~36.1%),夏、秋季发生干旱的频率最高。(3)干旱事件持续时间呈不显著的减少趋势,长时间尺度干旱事件平均持续时间、最长持续时间以及下降速度均大于短时间尺度。(4)降水集中程度增大会导致SPI1减小,增加干旱发生的可能性。典型极端降水可能会降低干旱发生的概率。 展开更多
关键词 降水 干旱 标准化降水指数(SPI) 大理河流域
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黄土区植被恢复对土壤水文物理性质的影响 被引量:5
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作者 刘卓昕 高鹏 +2 位作者 穆兴民 邱德勋 丁莹莹 《水土保持研究》 CSCD 北大核心 2023年第6期206-213,共8页
[目的]阐明黄土高原长期退耕还林(草)对土壤水文物理性质的影响,有利于完善黄土高原土壤水文研究,为黄土高原后续生态恢复提供理论依据。[方法]通过采样分析和原位双环入渗试验,针对不同植被恢复类型的土壤有机质、容重、孔隙度、含水... [目的]阐明黄土高原长期退耕还林(草)对土壤水文物理性质的影响,有利于完善黄土高原土壤水文研究,为黄土高原后续生态恢复提供理论依据。[方法]通过采样分析和原位双环入渗试验,针对不同植被恢复类型的土壤有机质、容重、孔隙度、含水量以及入渗性能等土壤水文物理性质进行了分析。[结果]植被恢复对土壤物理性质影响显著(p<0.05),造成的变化在0—40 cm土层表现得最为明显,有机质、孔隙度和>0.25 mm水稳性团聚体含量显著增加,容重显著降低。退耕还林(草)增强了土壤的入渗能力,相较于农地,绥德和神木草地的初始入渗分别增加了50%和31%;绥德和神木地区的草地、灌木、林地的稳定入渗速率分别增加了76%,11%,19%和53%,128%和58%。土壤稳定入渗和平均入渗与容重呈显著负相关关系(p<0.05),与总孔隙度、毛管孔隙度(p<0.05)和有机质含量(p<0.01)呈显著正相关。[结论]植被恢复对土壤水文物理性质影响显著,土壤入渗性能显著提高,有机质含量、容重和孔隙度对入渗性能有显著影响。 展开更多
关键词 植被恢复 土壤水文物理性质 黄土高原
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模拟降雨条件下垄沟坡度对溶解态氮磷流失的影响 被引量:1
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作者 扈晓碟 张含玉 +3 位作者 刘前进 徐相忠 邱德勋 马良 《水土保持学报》 CSCD 北大核心 2019年第6期41-46,共6页
为揭示不同垄沟坡度对径流中溶解态氮、磷流失的影响,采用人工模拟降雨试验,设置4个垄沟坡度处理(0°,9°,18°和27°),研究了不同垄沟坡度对径流中速效磷(PO4^3-—P)、硝态氮(NO3^-—N)和铵态氮(NH4^+—N)浓度和流失... 为揭示不同垄沟坡度对径流中溶解态氮、磷流失的影响,采用人工模拟降雨试验,设置4个垄沟坡度处理(0°,9°,18°和27°),研究了不同垄沟坡度对径流中速效磷(PO4^3-—P)、硝态氮(NO3^-—N)和铵态氮(NH4^+—N)浓度和流失量的影响;并利用Inorganic—N/PO4^3-—P、NO3^-—N/PO4^3-—P和NH4^+—N/PO4^3-—P 3种氮磷比,评价不同处理的富营养化风险。结果表明:(1)在降雨过程中,4个垄沟坡度处理径流中PO4^3-—P、NO3^-—N和NH4^+—N浓度随时间均呈锯齿状变化;其流失量随时间变化均呈先增加后以锯齿状变化的趋势,且波动幅度大,最大值(16.60,1020.73,48.35 mg)分别出现在垄沟坡度为0°,0°和9°处理。(2)4个垄沟坡度处理间相比较,径流中PO43-—P和NH4+—N流失量均表现为0°>9°>27°>18°,其浓度最大值(0.50,1.08 mg/L)和最小值(0.37,0.76 mg/L)均分别出现在垄沟坡度为9°和18°处理;而径流中NO3-—N浓度和流失量均在垄沟坡度0°处理时为最大值(30.68 mg/L和64.16 mg/m^2),18°处理时为最小值(21.78 mg/L和42.22 mg/m^2)。(3)Inorganic—N/PO4^3-—P率和NH4^+—N/PO4^3-—P率表明4个垄沟坡度处理径流中均存在一定的富营养化风险。其中,垄沟坡度为0°处理的径流富营养化风险水平最高,27°处理的径流富营养化风险水平最低。研究结果可为横坡垄作的水土流失及养分流失评价、预测以及防治提供科学依据。 展开更多
关键词 横坡垄作 垄沟坡度 模拟降雨 氮磷流失 富营养化风险
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Application of the InVEST model for assessing water yield and its response to precipitation and land use in the Weihe River Basin, China 被引量:5
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作者 WU Changxue qiu dexun +2 位作者 GAO Peng MU Xingmin ZHAO Guangju 《Journal of Arid Land》 SCIE CSCD 2022年第4期426-440,共15页
With realizing the importance of ecosystem services to society, the efforts to evaluate the ecosystem services have increased. As the largest tributary of the Yellow River, the Weihe River has been endowed with many e... With realizing the importance of ecosystem services to society, the efforts to evaluate the ecosystem services have increased. As the largest tributary of the Yellow River, the Weihe River has been endowed with many ecological service functions. Among which, water yield can be a measure of local availability of water and an index for evaluating the conservation function of the region. This study aimed to explore the temporal and spatial variation of water yield and its influencing factors in the Weihe River Basin(WRB), and provide basis for formulating reasonable water resources utilization schemes. Based on the InVEST(integrated valuation of ecosystem services and tradeoffs) model, this study simulated the water yield in the WRB from 1985 to 2019, and discussed the impacts of climatic factors and land use change on water yield by spatial autocorrelation analysis and scenario analysis methods. The results showed that there was a slight increasing trend in water yield in the WRB over the study period with the increasing rate of 4.84 mm/10a and an average depth of 83.14 mm. The main water-producing areas were concentrated along the mainstream of the Weihe River and in the southern basin. Changes in water yield were comprehensively affected by climate and underlying surface factors. Precipitation was the main factor affecting water yield, which was consistent with water yield in time. And there existed significant spatial agglomeration between water yield and precipitation. Land use had little impact on the amount of water yield, but had an impact on its spatial distribution. Water yield was higher in areas with wide distribution of construction land and grassland. Water yield of different land use types were different. Unused land showed the largest water yield capacity, whereas grassland and farmland contributed most to the total water yield. The increasing water yield in the basin indicates an enhanced water supply service function of the ecosystem. These results are of great significance to the water resources management of the WRB. 展开更多
关键词 water yield InVEST model Weihe River Basin Geoda model scenario analysis
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Spatial-temporal Analysis and Prediction of Precipitation Extremes: A Case Study in the Weihe River Basin, China 被引量:4
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作者 qiu dexun WU Changxue +2 位作者 MU Xingmin ZHAO Guangju GAO Peng 《Chinese Geographical Science》 SCIE CSCD 2022年第2期358-372,共15页
Extreme precipitation events bring considerable risks to the natural ecosystem and human life.Investigating the spatial-temporal characteristics of extreme precipitation and predicting it quantitatively are critical f... Extreme precipitation events bring considerable risks to the natural ecosystem and human life.Investigating the spatial-temporal characteristics of extreme precipitation and predicting it quantitatively are critical for the flood prevention and water resources planning and management.In this study,daily precipitation data(1957–2019)were collected from 24 meteorological stations in the Weihe River Basin(WRB),Northwest China and its surrounding areas.We first analyzed the spatial-temporal change of precipitation extremes in the WRB based on space-time cube(STC),and then predicted precipitation extremes using long short-term memory(LSTM)network,auto-regressive integrated moving average(ARIMA),and hybrid ensemble empirical mode decomposition(EEMD)-LSTM-ARIMA models.The precipitation extremes increased as the spatial variation from northwest to southeast of the WRB.There were two clusters for each extreme precipitation index,which were distributed in the northwestern and southeastern or northern and southern of the WRB.The precipitation extremes in the WRB present a strong clustering pattern.Spatially,the pattern of only high-high cluster and only low-low cluster were primarily located in lower reaches and upper reaches of the WRB,respectively.Hot spots(25.00%–50.00%)were more than cold spots(4.17%–25.00%)in the WRB.Cold spots were mainly concentrated in the northwestern part,while hot spots were mostly located in the eastern and southern parts.For different extreme precipitation indices,the performances of the different models were different.The accuracy ranking was EEMD-LSTM-ARIMA>LSTM>ARIMA in predicting simple daily intensity index(SDII)and consecutive wet days(CWD),while the accuracy ranking was LSTM>EEMD-LSTM-ARIMA>ARIMA in predicting very wet days(R95 P).The hybrid EEMD-LSTM-ARIMA model proposed was generally superior to single models in the prediction of precipitation extremes. 展开更多
关键词 precipitation extremes space-time cube(STC) ensemble empirical mode decomposition(EEMD) long short-term memory(LSTM) auto-regressive integrated moving average(ARIMA) Weihe River Basin China
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棕壤与褐土击实容重对含水量的响应
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作者 邱德勋 张含玉 +3 位作者 姜自龙 刘前进 陈锦鸿 韩曜蔚 《土壤》 CAS CSCD 北大核心 2019年第6期1209-1215,共7页
土壤在农业机械或者夯实压力下,容重会发生变化,其变化的程度受到土壤含水量的影响。为揭示棕壤与褐土受力后容重变化对含水量的响应特征,对土壤在不同的含水量下进行击实试验。结果表明:随着击实能量的增大,棕壤容重迅速增大后趋于稳定... 土壤在农业机械或者夯实压力下,容重会发生变化,其变化的程度受到土壤含水量的影响。为揭示棕壤与褐土受力后容重变化对含水量的响应特征,对土壤在不同的含水量下进行击实试验。结果表明:随着击实能量的增大,棕壤容重迅速增大后趋于稳定,而褐土容重达到稳定状态较慢。两种土壤容重随含水量的变化,因击实次数不同而具有差异性。棕壤容重随含水量增加,总体呈先增大后小幅度减小趋势,但在较低击实次数下,含水量为88.3 g/kg时容重略微减小;褐土容重在击实次数较低时,随土壤含水量增加呈先减小后增大趋势,而在击实次数较高时,呈先减小后增大而后又减小趋势,在含水量136.5 g/kg时出现最大值。含水量与击实能量对土壤击实容重的影响存在差异。在耕作条件(容重≤1.6 g/cm^3)和工程条件(容重>1.6g/cm^3)下,影响棕壤击实容重的最主要因素分别为含水量和击实次数,而影响褐土击实容重的最主要因素均为击实次数。在耕作条件下,棕壤击实容重在较低含水量(<50 g/kg)下数值较低,且随击实次数增多,容重变化较小;褐土的较小容重出现在较低击实能量范围内(<90 kJ/m^3),且受含水量的影响较小。在工程条件下,当棕壤与褐土的含水量为150 g/kg左右时,获得较大容重所需的击实能量最低。 展开更多
关键词 容重 含水量 击实 棕壤 褐土
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Runoff characteristics and its sensitivity to climate factors in the Weihe River Basin from 2006 to 2018 被引量:2
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作者 WU Changxue Xu Ruirui +4 位作者 qiu dexun DING Yingying GAO Peng MU Xingmin ZHAO Guangju 《Journal of Arid Land》 SCIE CSCD 2022年第12期1344-1360,共17页
Exploring the current runoff characteristics after the large-scale implementation of the Grain for Green(GFG)project and investigating its sensitivities to potential drivers are crucial for water resource prediction a... Exploring the current runoff characteristics after the large-scale implementation of the Grain for Green(GFG)project and investigating its sensitivities to potential drivers are crucial for water resource prediction and management.Based on the measured runoff data of 62 hydrological stations in the Weihe River Basin(WRB)from 2006 to 2018,we analyzed the temporal and spatial runoff characteristics in this study.Correlation analysis was used to investigate the relationships between different runoff indicators and climate-related factors.Additionally,an improved Budyko framework was applied to assess the sensitivities of annual runoff to precipitation,potential evaporation,and other factors.The results showed that the daily runoff flow duration curves(FDCs)of all selected hydrological stations fall in three narrow ranges,with the corresponding mean annual runoff spanning approximately 1.50 orders of magnitude,indicating that the runoff of different hydrological stations in the WRB varied greatly.The trend analysis of runoff under different exceedance frequencies showed that the runoff from the south bank of the Weihe River was more affluent and stable than that from the north bank.The runoff was unevenly distributed throughout the year,mainly in the flood season,accounting for more than 50.00%of the annual runoff.However,the trend of annual runoff change was not obvious in most areas.Correlation analysis showed that rare-frequency runoff events were more susceptible to climate factors.In this study,daily runoff under 10%-20%exceeding frequencies,consecutive maximum daily runoff,and low-runoff variability rate had strong correlations with precipitation,aridity index,and average runoff depth on rainy days.In comparison,daily runoff under 50%-99%exceeding frequencies,consecutive minimum daily runoff,and high-runoff variability rate had weak correlations with all selected impact factors.The sensitivity analysis results suggested that the sensitivity of annual runoff to precipitation was always higher than that to potential evaporation.The runoff about 87.10%of the selected hydrological stations were most sensitive to precipitation changes,and 12.90%were most sensitive to other factors.The spatial pattern of the sensitivity analysis indicated that in relatively humid southern areas,runoff was more sensitive to potential evaporation and other factors,and less sensitive to precipitation. 展开更多
关键词 daily runoff climate-related factors PRECIPITATION potential evaporation correlation analysis sensitivity analysis Weihe River Basin
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