三江平原粮食作物生产水足迹时空特征及影响因素

水足迹是评价人类活动对水资源开采和水环境污染程度的重要方法,对农作物生长过程的绿水足迹、蓝水足迹和灰水足迹进行量化和分析,可以为农业用水综合评价和用水管理提供指导。以三江平原为研究区域量化粮食作物生产水足迹的时空特征,揭示粮食生产对区域水资源的占用情况,并分析水足迹的影响因素。结果表明:(1)三江平原粮食生产水足迹总量在2005-2018年间呈显著增加趋势,其中绿水足迹、蓝水足迹和灰水足迹在水足迹总量中的占比历年平均为28%、8%和64%;(2)粮食生产水足迹空间差异明显,在地市尺度,佳木斯市水足迹最高,占三江平原总量的47%,在县区尺度,富锦市、依兰县和桦南县是水足迹热点地区;(3)只考虑蓝水足迹,粮食生产给三江平原水资源造成轻度压力,而同时考虑蓝水和灰水足迹,粮食生产给三江平原水资源造成重度压力;各地市间水资源压力有较大差异,其中佳木斯市负担了该区域将近一半的粮食产量,水资源压力最高,鹤岗市则水资源压力最低;(4)降雨量、灌溉水利用效率、化肥施用量、粮食种植结构和作物单产水平等都会影响粮食作物生产水足迹,其中蓝水足迹响应种植结构的变化最敏感,灰水足迹响应化肥施用量的变化最敏感,而水足迹总量响应作物单产水平的变化最敏感。因此,建议减少化肥施用量、提高作物单产水平和优化作物种植结构纳入区域水资源可持续管理之中。     

基于投入产出方法的甘肃省水足迹及虚拟水贸易研究

随着社会化进程的加快,地处西北内陆的甘肃省正面临日益严峻的水资源短缺危机,社会经济发展受到一定程度的制约,水生态环境也呈现出恶化的趋势。水足迹是近年来提出的衡量人类活动对于水生态系统影响的指标,能够帮助决策者制定水资源管理及保护的政策,从而实现地区水资源的可持续利用。运用单区域投入产出方法计算并分析了甘肃省1997、2002和2007年第一产业、第二产业和第三产业部门的虚拟水强度、水足迹以及虚拟水贸易情况。结果显示:(1)甘肃省第一产业的虚拟水强度最高,但呈现出逐年下降的趋势,水足迹也因此有所下降;(2)虚拟水贸易方面,甘肃省以虚拟水净出口为主,尤其是第一产业,每年虚拟水净出口量约全省总水资源量的10%。建议甘肃省继续巩固已有的节水成果,调整产业结构,大力发展节水型产业和高新技术产业。同时建议适当调整贸易格局,合理控制虚拟水出口,以缓解当地水资源短缺危机,保障地区水安全与生态安全。     

科尔沁沙地4种植物抗旱性的比较研究

对科尔沁沙地小叶锦鸡儿,紫穗槐,差巴嘎蒿和胡枝子4种植物的若干水分生理生态指标进行了测定。结果表明,小叶锦鸡儿具有低水势,高水力和束缚水／自由水比及水分利用效率,抗旱性强;紫穗槐的各项指标与小叶锦鸡儿相反,抗旱性最差;差巴嘎蒿虽然水势较高,但它的持水力高,束缚水／自由水比和水分利用效率都较高,抗旱性也较强,但次于小叶锦鸡儿;胡枝子的水势和持水力较低,束缚水／自由水比及水分利用效率一般,它的抗旱性强于紫穗槐,但比差巴嘎蒿差。     

基于多区域投入产出分析的京津冀地区虚拟水核算

通过贸易与消费调控实现区域水资源优化配置已成为缓解地区水资源压力的途径之一。跨区域投入产出分析可为地区间虚拟水贸易战略提供依据。基于2012年京津冀地区投入产出表与生产用水量构建了跨地区虚拟水核算模型,计算了隐含在经济贸易中的虚拟水总量及各地区各部门的直接用水系数、完全用水系数和拉动系数,分析了各部门虚拟水进出口情况,识别了重点耗水部门。结果表明:京津冀地区呈现虚拟水净出口状态,其中净出口部门主要为北京的服务与交通业,河北的农业和制造业。京津冀的农业、矿业和水供应业在生产过程中直接消耗水量大,应注重提升用水效率及节水技术的开发;三地制造业、建筑业和服务与交通业的平均拉动系数较大,这说明其他部门生产活动对该部门依赖性较大,其单位产出的提高将带动整个地区更多虚拟水量的投入。此外,河北的农业和制造业为京津冀各部门输送了大量虚拟水,为各部门生产提供了支撑,是节水的重点部门,应着重调整其产业结构,并从直接和间接用水两方面入手减少水资源消耗。计算了京津冀地区不同部门的直接、间接水资源消耗、水资源消耗拉动系数,以及部门间的虚拟水贸易情况,结果可为该地区部门间水资源配置和虚拟水战略的制定提供基础。     

“生态活水”治水原理与扬州黑臭水体治理

为探索黑臭水体治理的根本途径,在研究自然水体净化功能,分析水体黑臭根本原因和直接原因的基础上,深入阐述了“生态活水”的科学内涵和生态功能,全面揭示了“生态活水”治水的科学原理和技术优势。“生态活水”治水为原位原生态治水,通过水体快速复氧,创建活水微生态系统,并借助微速循环流水的载体作用,实现持续高效净化。扬州黑臭水体治理的实践表明:采用“生态活水”方法治水后3～5 d可以完全消除黑臭,并将黑臭水体转化为“绿水”;15～20 d后水质达国家地表水Ⅲ类水标准。说明“生态活水”治水技术是一种占用资源少、设备投资省、治污速度快、运行成本低、治水效果好、标本兼治的可持续治水技术体系。     

Virtual water and water footprints do not provide helpful insight regarding international trade or water scarcity

Many authors have estimated the virtual water content of good and services traded internationally, and many have calculated national water footprints that account for the volumes of virtual water imported and exported. Some authors have suggested that international trade of virtual water has been harmful to selected exporting countries with limited water endowments. Some suggest also that current patterns of international trade should be rearranged to make better use of global water resources. Yet, countries do not actually trade in virtual water. They trade in goods and services for which water is one of many inputs. Wise choices regarding water resources and smart strategies regarding international trade cannot be determined by focusing on water alone. The notions of virtual water and water footprints are not helpful indicators of optimal strategies regarding water resources, particularly when considering issues such as water scarcity or international trade. I describe four perspectives regarding virtual water and water footprints, with the goal of demonstrating the inadequacies of these notions in policy discussions and in efforts to determine the optimal allocation and use of water resources. The four perspectives are: (1) international trade should not be modified or regulated to reflect the virtual water content of traded commodities or water footprints in the countries of trading partners, (2) countries do not save water by engaging in virtual water trade, (3) consumers in one country cannot alleviate water scarcity or improve water quality in other countries, and (4) water footprints are not analogous to carbon or ecological footprints.     

内陆河干旱区生态需水分析

根据水分驱动生态演变模型 ,以水分运动和补给条件 ,研究了内陆河平原生态系统的需水结构。生态需水分为过渡带生态需水 ,绿洲生态需水 ;绿洲生态需水又进一步分为天然绿洲生态需水和人工绿洲生态需水。通过流域水分平衡和地面观测资料确定了生态圈层结构的水分需求 ,以及降水与径流对水分需求的补给比例。生态需水的分析计算 ,类似于供需平衡分析。从植物生理角度分析生态需水 ,得到天然植被的总腾发量 Et,作为植被生态需水总量。各典型天然植被的 Et通过实验资料获得。将植被和水面的总生态需水量扣除有效降水补充的部分 ,即为径流性生态需水量 GE。另一方面 ,以流域为单元进行降水和径流统一考虑的水分综合平衡 ,进行生态可利用水量分析。得到生态系统可能实际利用的径流性水资源量 GR。　　将生态需水量 GE与生态系统可能实际利用的水资源量 GR进行平衡分析 ,计算实际生态耗水 ,并分析盐碱地无效耗水。根据 2 0 2 0年生态状态情景分析 ,作出了 2 0 2 0年生态需水与生态系统结构演变的预测     

西部干旱区生态需水的规律及特点——以塔里木河下游绿色走廊为例

天然植被蒸散耗水量小,水分有效利用程度高,生态需水可塑性及水质变幅较大等是生态需水的主要特点．保护塔里木河下游绿色走廊的生态需水量,主要是指大西海子以下自然植被的需水量．即地下水位恢复总水量和全河段生态总维持水量,前者主要包括水位恢复水量、侧向排泄量及河道蒸发水量．2005年泄水目标为阿尔干,生态总需水量为恢复大西海于至阿尔干地下水的总水量,该水量为13．20×10^8m^3,年均需水量为2．64×10^8m^3．2010年泄水目标及植被保护目标都是台特玛湖,生态总需水量包括恢复阿尔干至台特玛湖段地下水位的水量以及维持大西海子至台特玛湖段生态的维持水量,该水量为18．32×10^8m^3,年均需水量为3．66×10^8m^3．2010—2030年的生态总需水量包括每年维持大西海子至台特玛湖段生态的总维持水量,同时也包括增加植被18．67×10^4hm^2所需要的水量,20年生态总需水量为139．00×10^8m^3,年均需水量为6．95×10^8m^3．通过一系列措施保证生态用水,是干旱区生态建设的关键．     

基于ESTDA模型的中国水生态足迹及水生态压力评价

基于水足迹视角,测度了中国31个省份2000-2018年的水生态足迹广度、深度及水生态压力,采用ESTDA框架对其时空动态特征进行分析。结果表明：①研究期内,中国水生态足迹总量呈波动上升态势;水生态承载力波动幅度较大,空间分布格局整体呈现自东南向西北逐渐较少的趋势。②水生态足迹广度与水生态承载力呈同步变化趋势,整体上已接近水资源可提供的流量资本上限,各省市水生态足迹深度差异较大。③研究期内,水生态压力指数小于1的区域与水生态足迹深度为1的区域相吻合,水生态压力指数大于1的区域主要分布在华北及西北地区。④LISA时间路径表明,水生态足迹广度、深度及水生态压力的整体空间格局均具有较强的稳定性;三者的局部空间结构在空间依赖方向上的稳定性依次加强;空间格局演化的空间整合性呈现水生态足迹深度 > 水生态压力 > 水生态足迹广度,空间上,水生态足迹广度正向协同增长省份主要集中于南方省份,而水生态足迹深度和水生态压力正向协同增长区则分布于华北、西北地区;各要素的空间分布格局表现出较强的路径依赖及锁定特征。     

基于水足迹理论的煤制油产业布局评价

煤制油是我国应对石油危机的重要途径之一,但其高耗水的特点使其备受争议。利用水足迹理论对全国五大煤炭基地2015年规划的煤制油产业进行了蓝水足迹和灰水足迹的测算,分析了煤制油产业对这些区域水资源的耗用情况及冲击程度。结果显示,神东、晋东和新疆伊犁3个基地的煤制油产业蓝水足迹超过了1亿t、灰水足迹超过了3亿t,其中神东地区作为最大的煤制油产地两项数值分别达到1.9亿t和4.1亿t与当地水资源总量对比,宁东地区煤制油耗水冲击最大,占当地水资源总量的28.2%;新疆伊犁地区比例最小,为0.36%。通过对这5个煤炭基地以区域为尺度的水足迹结构分析和评价比较,得出了两种煤制油工艺的水资源消耗差异,并且为煤制油产业在五大基地的合理布局给出了依据,与此同时为接下来煤制油产业的技术革新和流程优化也提出了相应的建议。     

A simple approach to assess water scarcity integrating water quantity and quality

Water scarcity has become widespread all over the world. Current methods for water scarcity assessment are mainly based on water quantity and seldom consider water quality. Here, we develop a simple approach for assessing water scarcity considering both water quantity and quality. In this approach, a new water scarcity index is used to describe the severity of water scarcity in the form of a water scarcity meter, which may help to communicate water scarcity to a wider audience. To illustrate the approach, we analyzed the historical trend of water scarcity for Beijing city in China during 1995–2009. The results show that Beijing made a huge progress in mitigating water scarcity, and that from 1999 to 2009 the blue and grey water scarcity index decreased by 59% and 62%, respectively. These achievements were made through great efforts of water-saving measures and wastewater treatment. Despite this progress, we demonstrate that Beijing is still characterized by serious water scarcity due to both water quantity and quality. The water scarcity index remained at a high value of 3.5 with a blue and grey water scarcity index of 1.2 and 2.3 in 2009 (exceeding the thresholds of 0.4 and 1, respectively). As a result of unsustainable water use and pollution, groundwater levels continue to decline, and water quality shows a continuously deteriorating trend. To curb this trend, future water policies should further decrease water withdrawal from local sources (in particular groundwater) within Beijing, and should limit the grey water footprint below the total amount of water resources.     

热变性前后水合醛缩酶中水状态的热力学研究

 用差示扫描量热计,测定了不同水合态(水含量h从0.08g/g至2.50g /g)冻结的水合醛缩酶样品中冰的熔化温度和熔化焓,并计算出熔化熵。实验结果表明,变性前,水合醛缩酶中的水转化成四种状状:(1)不冻结水,(2)熔化焓和熔化温度均低了普通水的可冻结水,(3)熔化焓与普通水相同而熔化温度低于普通水的可冻结水,(4)熔化焓和熔化温度均与普通水相同的容积水。变性后,水合醛缩酶中的水可处于五种状态,即不冻结水,熔化焓低于普通水而熔化温度与普通水相同的可冻结水,以及熔化温度均低于普通水且彼此不相同的三种状态的可冻结水。实验还观察到,水合醛缩酶在热变性前后,水在这些态中的量是不同的。     

飞来峡水库水质现状及其向广州供水能力的探讨

水库供水(特别是对城市的供水)已成为缓解全球水资源供给不足的重要途径。于2001年至2003年的丰水期和枯水期调查分析了新建河流型水库-飞来峡水库的水质、浮游植物群落特征和营养状态。结果表明飞来峡水库水质良好,多数水质指标为地表水Ⅱ水质标准,其营养盐浓度、浮游植物的密度均较低,属于贫中营养。从近几年的水质变化来看,建库后,水质改善明显。通过对广州市饮用水源水水质现状及存在问题的分析,从水质和水量两方面探讨了飞来峡水水库作为广州优质水源地的优势。由于来水量大,水库水质净化能力强,飞来峡水库水质和水量均有保证,可作为广州市重要水源地之一。但今后,在流域管理和水土保持工作更应重视和加强。     

Water structure changes induced by ceramics can be detected by increased permeability through aquaporin

Aquporins are intrinsic membrane proteins that function as water channel to transport water and/or mineral nutrients across biological membranes. In this study, we aimed to clarify whether water structure can be changed by the presence of ceramics and whether such a change can be determined by aquaporin. First, we confirmed that ceramics could transform tap water into active tap water by increasing water permeability through aquaporin. We also found that this change in water permeability by treatment with ceramics occurred in distilled water. The distilled water was determined to exhibit the same aquaporin permeability as the original tap water. Our data indicate that the aquaporin permeability of water can be changed by severe physical shocks, such as slapping and sonication, which is consistent with the implication that the aquaporin permeability is closely related to the structure of the water. In this study, using aquaporins, we first reported that the treatment of water with ceramics can affect the structure of water, and the water can retain the structure for a given period under certain condition     

农产品水足迹研究进展

水是人类生产生活的重要资源,科学合理地评价人类活动对水资源的影响是实现水资源可持续利用的重要保障.水足迹概念的提出创新性地将人类活动消耗的水资源区分为绿水、蓝水和灰水,拓展了水资源可持续利用的评价思路.基于虚拟水(VW)的水足迹理论和基于生命周期(LCA)的水足迹理论将水质与水量的概念相结合,成为了农业水资源管理研究的热点内容.基于VW的水足迹理论主要包括绿水足迹、蓝水足迹和灰水足迹的计算,以及水环境可持续性评价,而基于LCA的水足迹理论体现了水资源的消耗和污染及其对环境造成的综合影响.本文详细介绍了这两种水足迹理论的计算方法与环境可持续评价的研究进展,对比分析两种水足迹理论在描述农产品生产用水及其环境影响方面的差异性,并对其研究前景进行了展望.     

Water resources stress assessment and risk early warning–a case of Hebei Province China

In most parts of China, water resources development and utilization has reached or exceeded the international warning level, especially in the northern arid and semi-arid regions, the serious water stress have aroused worldwide concerns. Many issues of water resources are closely and some inseparably associated with human activities. In this study, the water footprint (WF) and related indicators were applied as comprehensive indicators to assess real water use by humans from the consumption perspective. A Fuzzy Comprehensive Evaluation Model (FCE) was used for the evaluation in its role to assess water stress. And the index system of water stress assessment including four aspects, namely water supply and demand balance, socio-economy, agricultural production and ecological environment was established. Taking the case of Hebei province of China where there is serious conflict between water supply and demand, water stress assessment of all eleven administrative areas for the period 2000–2013 was analyzed. The findings showed that water stress was denoted by three levels, namely high water stress (red zone), general water stress (yellow zone) and low water stress (blue zone), which lays the foundation of the further research on water risk warning. According to the results of water stress assessment and the socio-economic development trends of Hebei, a Markov Chain Risk Warning model was built to describe the risk state of water system and to predict the transition probability of future states. This was intended to focus on the possibility that water stress levels might change into higher water stress level. The current study aims at extending earlier research by making a first step from water footprint estimation towards water stress assessment and providing reference for scientific management of water resources in arid and semi-arid regions.     

水足迹研究进展

水为生命之源,水资源的合理分配与科学管理是区域可持续发展与流域综合管理的核心环节;水足迹作为一种全面核算人类活动对水资源真实占用的综合指标,将人类消费终端与水资源利用密切关联,为维护流域水资源安全、提高区域水资源利用效率提供了重要的科学依据,已成为当前国际水资源管理的前沿研究领域。在明确水足迹及水资源生态足迹相关概念的基础上,对比分析了水足迹与生态足迹、水资源生态足迹模型的异同,明晰了过程、产品及区域等不同研究对象的水足迹核算方法,系统梳理了产品和区域水足迹评价、基于水足迹的区域水资源安全研究、区域水足迹可持续性分析等水足迹主要研究内容的近今进展,并展望了进一步的重点研究方向,即水足迹综合研究、水足迹评价不确定性分析、水足迹与物质流核算的关联研究,以及基于足迹整合的可持续发展多维测度等。     

Water mites as indicators of natural aquatic ecosystems of the coastal dunes of the Netherlands and northwestern France

A large number of coastal dune waters in the Netherlands and northwestern France have been investigated for the occurrence of water mites. Dune waters turned out to be very rich in water mite species. In the Dutch dunes, 110 species of water mites have been found; this is 50 % of the total number of water mite species present in the Netherlands. In the French dunes 64 species have been found. The water mites most characteristic of the coastal dunes are the temporary water species. Dune areas with a high-lying hinterland have a water mite composition much different from dune areas with a low-lying hinterland. This can be explained by the existence of a very different hydrology. During the last century human activity affected the ground water of dunes. Afforestation and extraction of ground water for drinking water purposes caused a lowering of the ground water table. As a result, many dune slacks dried out. Moreover, the infiltration of river water caused an eutrophication of the ground water. Nowadays, the dunes most rich in typical water mite species are the dunes in which neither infiltration of river water nor extraction for drinking water purposes, occur. It can be concluded that water mites are good indicators for dune areas with a natural hydrology.     

不同供水条件下侧柏和刺槐幼树的蒸腾耗水与土壤水分应力订正

采用旱棚人工控水,对侧柏、刺槐不同水量全生长期均衡供水条件下,2～3年生幼树的生理需水规律、蒸腾耗水与土壤水分的关系进行了研究.结果表明,刺槐蒸腾耗水量随土壤供水能力的增大而增加.其中以生长前期和生长盛期耗水为主,约占年蒸腾耗水量的80.5%;刺槐年均生理需水量是侧柏的5.13倍.侧柏蒸腾耗水量在土壤相对含水率为40%～100%有一峰值.当土壤相对含水率≤87.84%时,蒸腾耗水量随土壤相对含水率增加而增大;反之则减小.侧柏蒸腾耗水量以生长盛期最大,约占年蒸腾量的46.27%,生长后期次之,生长前期较小.并求出了两树种蒸腾耗水的土壤水分应力订正函数及在非充分供水条件下实际蒸腾耗水的时间-水分函数.     

不同生育期玉米叶片光合特性及水分利用效率对水分胁迫的响应

利用大型移动防雨棚开展了玉米水分胁迫及复水试验,通过分析玉米叶片光合数据,揭示了不同生育期水分胁迫及复水对玉米光合特性及水分利用效率的影响。结果表明:水分胁迫导致玉米叶片整体光合速率、蒸腾速率和气孔导度下降以及光合速率日变化的峰值提前;水分胁迫后的玉米叶片蒸腾速率、光合速率和气孔导度为适应干旱缺水均较对照显著下降,从而提高了水分利用效率,缩小了与水分充足条件下玉米叶片的水分利用效率差值;在中度和重度水分胁迫条件下,玉米叶片的水分利用效率降幅低于光合速率、蒸腾速率和气孔导度的降幅, 有时甚至高于正常供水条件下的水分利用效率;适度的水分胁迫能提高玉米叶片的水分利用效率,从而增强叶片对水分的利用能力,抵御干旱的逆境;水分亏缺对玉米光合速率、蒸腾速率及水分利用效率的影响具有较明显滞后效应,干旱后复水,光合作用受抑制仍然持续;水分胁迫时间越长、胁迫程度越重,叶片的光合作用越呈不可逆性;拔节-吐丝期水分胁迫对玉米叶片光合作用的逆制比三叶-拔节期更难恢复。