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| 1 | 基于FEFLOW和GIS技术的矿区地下水动态模拟及预测显示文摘矿区地下水动态研究是山西亟待解决的重大需求问题。针对山西矿区水资源短缺与水环境恶化等现状,通过分析气象、水文、地质地貌、开采现状等监测数据资料,以FEFLOW模型和GIS技术为平台,构建山西矿区三维地下水数值模型,进行地下水动态研究,模拟并预测了4种不同情境下矿区地下水动态过程,从而定量分析采矿活动对地下水动态的影响,揭示矿区开采对地下水系统的作用机制。结果表明:当矿区开采强度提高10%、30%、50%时,地下水整体流场和运动趋势没有大的变化,但在矿区南部地下水流场发生突变,等值线形变,且在东南部形成一个水位变化剧烈的低水位带,迫使地下水流向发生偏转。水位分析表明采矿活动会造成地下水位整体下降,下降幅度与开采强度呈正相关关系。地下水系统均衡分析表明,当开采强度保持现状或提高10%,地下水系统仍然处于正均衡,补给量大于排泄量,当开采强度提高30%、50%时,系统转为负均衡状态,补给量小于排泄量,地下水水量大幅度减少。研究成果可为矿区制定合理的开采方案,保护矿区地下水资源提供参考依据,为有效遏制矿区水环境恶化、确保矿区水安全提供科技支撑。 | 李彩梅 杨永刚 秦作栋 邹松兵 李晋昌 | 2015 | 干旱区地理2015，38，2： | 18 |
| 2 | 基于元数据分析的西北干旱区生态地下水位埋深及其影响因素显示文摘综合现有文献研究成果,基于元数据分析方法研究不同植被的适宜、极限生态地下水位埋深。选择乔木、灌木和草本等3种植被类型中的13种植物,分析适宜、极限生态地下水位埋深的统计分布、生物多样性和丰富度指数,推求生态地下水位埋深与植物根系和土壤质地的关系,得出:西北地区适宜和极限生态地下水位埋深均值分别为2.9、5.5m,控制范围分别为2.3~3.9、4.0~7.2m;适宜、极限生态地下水位埋深与植物根系具有显著的相关关系,适宜生态地下水位埋深还取决于植物根系伸展速率与地下水位埋深下降速率的相对关系;土壤质地控制毛细管上升高度及地下水位埋深以上水分供给能力,是确定生态地下水位埋深的重要因子。 | 张阳阳 陈喜 高满 刘秀强 | 2020 | 南水北调与水利科技(中英文)2020，18，5： | 10 |
| 3 | 荒漠河岸胡杨林生态系统能量分配及蒸散发显示文摘生态输水工程使得黑河下游地区荒漠河岸林的面积得到了恢复,为进一步巩固生态恢复的成果,非常有必要深入研究胡杨林生态系统的水热交换过程及其对环境因子和人类活动的响应机理。基于涡度相关技术,对2013—2016年荒漠河岸胡杨林生态系统的水热交换过程进行了研究,得出的主要结论如下:(1)生长季生态系统的能量消耗以潜热通量为主,波文比为0.21;非生长季则以感热通量为主,波文比为3.61;春季和秋季的灌水过程,使得胡杨生长前期和后期的潜热通量值较高,直接影响着胡杨林生态系统的能量分配。(2)灌水的时间改变了潜热通量和蒸散发的季节变化过程,而灌水的量决定着春季和秋季潜热通量和蒸散量的年际差异。(3)2014—2016年,生态系统的年蒸散量和生长季蒸散量平均分别为1092 mm和932 mm。荒漠河岸胡杨林生态系统的蒸散量主要受系统水分状况(灌水量)及植物生长状况的影响。 | 马小红 冯起 | 2020 | 生态学报2020，40，23： | 7 |
| 4 | Evapotranspiration of a Populus euphratica Oliv. forest and its controlling factors in the lower Heihe River Basin,Northwest China显示文摘Evapotranspiration(ET) within an ecosystem is crucial for the water-limited environment that currently lacks adequate quantification in the arid region of Northwest China, mainly covered by phreatophytes, such as the Populus euphratica Oliv. tree and the Tamarix ramosissima Ledeb. shrub species. Accordingly, ET was measured for an entire year using eddy covariance(EC) in P. euphratica stands in the lower Heihe River Basin, Northwest China. During the growing season,the total ET was 850 mm, with a mean of 4.0 mm/d, which is obviously more than that observed at tree-level and standlevel scales, which was likely due to the different level of soil evaporation induced by irrigation via water conveyance.Factors associated with ET fall into either environmental or plant eco-physiological categories. Environmental factors account for at least 79% variation of ET, and the linear relationship between ET and the groundwater table(GWT) revealed the potential water use of P. euphratica forests under the non-water stress condition with the GWT less than 3 m deep.Plant eco-physiological parameters, specifically the leaf area index(LAI), have direct impact on the seasonal pattern of ET, which provides a valuable reference to the wide-area estimates of ET for riparian forests by using LAI. In conclusion,P. euphratica forests have high water use after water conveyance, which may be the result of long-term adapting to local climates and limited water availability. | TengFei Yu Qi Feng JianHua Si XiaoYou Zhang ChunYan Zhao | 2017 | Research in Cold and Arid Regions2017，9，2： | 6 |
| 5 | Groundwater evapotranspiration under psammophilous vegetation covers in the Mu Us Sandy Land, northern China显示文摘Groundwater is a significant component of the hydrological cycle in arid and semi-arid areas. Its evapotranspiration is an important part of the water budget because many plants are groundwater-dependent. To restore the degraded ecosystems, the need is pressing to further our understanding of the groundwater evapotranspiration(ET_g) in arid and semi-arid areas. This study employed the White method to estimate ET_g at four sites in the Mu Us Sandy Land in northern China, and the four sites are covered by Salix psammophila(SP site), Artemisia ordosica(AO site), Poplar alba(PA site), and Carex enervis(CE site), respectively. The depth of groundwater table and the duration of drainage were taken into account in calculating the specific yield(S_y) to improve the accuracy of the ET_g estimats. Our results showed that from late May to early November 2013 the ET_g were 361.87(SP site), 372.53(AO site), 597.86(PA site) and 700.76 mm(CE site), respectively. The estimated ET_g rate was also species-dependent and the descending order of the ET_g rate for the four vegetation was: C. enervis, P. alba, A. ordosica, and S. psammophila. In addition, the depth of groundwater table has an obvious effect on the ET_g rate and the effect varied with the vegetation types. Furthermore, the evapotranspiration for the vegetation solely relying on the water supply from unsaturated layers above the groundwater table was much less than that for the vegetation heavily relying on the water supply from shallow aquifers. | CHENG Donghui DUAN Jibo QIAN Kang QI Lijun Yang Hongbin CHEN Xunhong | 2017 | Journal of Arid Land2017，9，1： | 4 |
| 6 | How changes of groundwater level affect the desert riparian forest ecosystem in the Ejina Oasis,Northwest China显示文摘Groundwater is a key factor controlling the growth of vegetation in desert riparian systems. It is important to recognise how groundwater changes affect the riparian forest ecosystem. This information will not only help us to understand the ecological and hydrological process of the riparian forest but also provide support for ecological recovery of riparian forests and water-resources management of arid inland river basins. This study aims to estimate the suitability of the Water Vegetation Energy and Solute Modelling(WAVES) model to simulate the Ejina Desert riparian forest ecosystem changes,China, to assess effects of groundwater-depth change on the canopy leaf area index(LAI) and water budgets, and to ascertain the suitable groundwater depth for preserving the stability and structure of desert riparian forest. Results demonstrated that the WAVES model can simulate changes to ecological and hydrological processes. The annual mean water consumption of a Tamarix chinensis riparian forest was less than that of a Populus euphratica riparian forest, and the canopy LAI of the desert riparian forest should increase as groundwater depth decreases. Groundwater changes could significantly influence water budgets for T. chinensis and P. euphratica riparian forests and show the positive and negative effects on vegetation growth and water budgets of riparian forests. Maintaining the annual mean groundwater depth at around 1.7-2.7 m is critical for healthy riparian forest growth. This study highlights the importance of considering groundwater-change impacts on desert riparian vegetation and water-balance applications in ecological restoration and efficient water-resource management in the Heihe River Basin. | HaiYang Xi JingTian Zhang Qi Feng Lu Zhang JianHua Si TengFei Yu | 2019 | Research in Cold and Arid Regions2019，11，1： | 1 |
| 7 | 厄立特里亚Zara地区Koka金矿开采的地下水资源可持续性分析显示文摘在非洲干旱性气候条件下,水资源的补给量稀缺,做到地下水资源的有效平衡极其重要。在分析Zara科卡金矿水文地质条件的基础上,建立了准三维有限差分地下水流模型,模拟预测了科卡金矿开采期间和封场后,在丰水、枯水和平水3种气候条件下矿山供水对地下水水位降深的影响,并对有、无矿山供水条件下的地下水水位降深进行了对比分析。模拟结果表明:前1~3 a,日供水量约0.97×10~4m^3/a,在4~7 a,日供水量约在1.01×10~4m^3/a,矿山供水开采不会引起当地地下水资源枯竭,且矿山关闭后,含水层水位会很快恢复;即使在增加矿山供水和枯水气候同时出现的最不利条件下,井场中心出现最大地下水位降深为1.0~1.2 m,且距离井场中心距离约2km的边缘区域,地下水位降深仅为0.2 m。模拟结果可为高温干旱地区矿山的供水开采提供科学依据。 | 何鑫 庞红璐 周泉吉 李文娟 闫鑫宇 林国庆 | 2017 | 水资源与水工程学报2017，28，5： | 1 |
| 8 | Comparable water use of two contrasting riparian forests in the lower Heihe River basin, Northwest China显示文摘Understanding forest ecosystem evapotranspiration(ET) is crucial for water-limited environments,particularly those that lack adequate quantified data such as the lower Heihe River basin of northwest China which is primarily dominated by Tamarix ramosissima Ledeb.and Populus euphratica Oliv.forests.Accordingly,we selected the growing season for 2 years (2012 and 2014) of two such forests under similar meteorological conditions to compare ET using the eddy covariance(EC) technique.During the growing seasons,daily ET of T.ramosissima ranged from 0.3 to 8.0 mm day^(-1) with a mean of 3.6 mm day^(-1),and daily ET of P.euphratica ranged from 0.9 to 7.9 mm day^(-1) with a mean of 4.6 mm day^(-1) for a total of 548 and 707 mm,respectively.The significantly higher ET of the P.euphratica stand was directly linked to high soil evaporation rates under sufficient water availability from irrigation.When the soil evaporation was disregarded,water use was comparable to two contrasting riparian forests,a P.euphratica forest with a total transpiration of 465 mm and a T.ramosissima forest with 473 mm.Regression analysis demonstrated that climate factors accounted for at least 80% of ET variation in both forest types.In conclusion,water use of the riparian forests was low and comparable in this arid region,that suggest the long-term plant adaptation to the local climate and conditions of water availability. | Tengfei Yu Qi Feng Jianhua Si Xiaoyou Zhang Haiyang Xi Chunyan Zhao | 2018 | Journal of Forestry Research2018，29，5： | 1 |
| 9 | 核素肾显像剂的制备和临床应用显示文摘 | 张立兴 程丙武 夏继红 | 2000 | 锦州医学院学报2000，21，1： | 0 |
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