Principles and technology for stepwise utilization of resources for mitigating deep mine heat hazards

As is well known, deep mines are hot. As mining depth increases, the temperature of the surrounding rock also increases. This seriously affects mine safety and production and has restricted the exploitation of deep coal resources. Therefore, reducing the working face temperature to improve working conditions by controlling these heat hazards is an urgent problem. Considering problems in cooling deep mines both domestically and abroad along with the actual conditions of the Zhangshuanglou coal mine, we propose a HEMS technology that uses heat resources from deep mines in a stepwise manner. HEMS means a high temperature ex-change machinery system. Mine inrush-water is used as a source of cooling. Twice the energy is extracted from the mine inrush water. Heat is used for building heating in the winter and cold water is used for cooling buildings in the summer. This opens a new technology for stepwise utilization of heat energy in deep mines. Energy conservation and reduced pollution, an improved environment and sustainable economic development are realized by this technique. The economic and social effects are obvious and illustrate a good prospect for the application and extension of the method.

Analysis on the Changes of Temperature and Heat Resources in Rural Area of Chaoyang in Western Liaoning

[Objective] The aim was to study the change characteristics of temperature and heat resources in rural area of Chaoyang in western Liaoning. [Method] Based on the data from rural meteorological station in Chaoyang in western Liaoning from 1966 to 2010, the change characteristics of temperature and heat resources in rural area in Chaoyang were analyzed by means of serial correlation and climate tendency method, so as to master its climate situation. [Result] The annual average value of daily average temperature, daily maximum temperature and daily minimum temperature in rural area of Chaoyang in western Liaoning from 1966 to 2010 showed fluctuation variation, and the annual average value of daily maximum temperature increased most obviously with the climatic tendency of 0.328 ℃/10 a and highest significant level, so it played an important role in temperature increase, next came daily average temperature (0.151 ℃/10 a), while there was no obvious decrease in daily minimum temperature. The average of daily maximum temperature in winter half year increased more obviously than that in summer half year, with the climatic tendency of 0.417 and 0.250 ℃/10 a, respectively; the trend of daily average temperature reached low significant level, and there was no obvious variation in daily minimum temperature. In addition, ≥10 ℃ accumulated temperature in rural area of Chaoyang in western Liaoning went up obviously, with the climatic tendency of 42.59 ℃·d/10 a, namely it increased by 192 ℃·d in recent 45 years. [Conclusion] The study could provide climatic reference for the adjustment of agriculture structure and varieties distribution.

Effect of Heat Resources Characteristic Change on Agriculture in Fuxin Area of Liaoning

The analysis on the trend change of heat resources serviced for the industrial structure adjustment of agriculture and the increase of agricultural economical income.The result showed that increase trend of heat resources in Fuxin region was obvious.≥0 ℃ first day trend advanced 12 d,and the interval days trend increased 17 d.Moreover,the accumulated temperature trend increased 396 ℃.≥10 ℃ first day trend advanced 7 d,and the final day trend delayed 9 d.Moreover,the interval days increased 15 d,and the accumulated temperature trend increased 350 ℃.The latest frost date trend advanced 10 d,and the first frost date trend delayed 12 d.Moreover,the frost-free period trend prolonged 23 d.On one hand,the increase of heat resources favored the adjustment of crops variety structure,the development of agricultural facilities,the change of agricultural measures,the improvement of multiple cropping indexes and the increase of agricultural economical income.On the other hand,it made that the agricultural pests shifted northward by passing the winter boundary,and the insect source radix increased.In addition,the heat resources increase would also cause that the soil potential evapotranspiration increased,and the precipitation utilization ratio decreased.Then,the agricultural production environment worsened,and the dry land agriculture,irrigated agriculture were threatened.It could be said that the advantages and disadvantages of climate warming and heat resources increase on the agricultural production both existed.

An Analysis on the Heat Resistance of Rice Germplasm Resources during Flowering Period

56 Chinese rice core germplasm resources,18 foreign rice germplasm resources and 6 restorer lines are subjected to high temperature stress during flowering period. Based on relative spikelet fertility rate,rice heat resistance is evaluated. The results show that different resistance to high temperature exists in different varieties,and 6 new rice varieties present high heat resistance.

Variation Characteristics of Heat Resources in Liaoning Province, China in Recent 60 Years and Their Impact on Meteorological Services

To study the temporal and spatial changes of heat resources to serve agricultural production and economic development. The climate data from 1958 to 2017 were selected, and the temporal and spatial changes of heat resources in Liaoning, China were analyzed by using the method of climate diagnosis and analysis. The results show that: the southern coastal area of Liaoning has the most heat resources, the northwestern hilly area and the eastern mountainous area the least, and the central plain area in the middle distribution pattern;compared with 1958-1980, 1981-2017 ≥0°C, ≥10°C accumulated temperature, etc. The value line is advanced 100-160km northward. The accumulated temperature of ≥0°C and ≥10°C in Liaoning experienced abrupt changes in climate in 1993 and 1994, and the climate abrupt change in the southern coastal area was earlier than that in the inland. , the increase in the northwestern hilly area and the eastern mountainous area is less than that in the central plain area and the southern coastal area. The study on the impact on meteorological services found that the increase or decrease of heat resources has a significant impact on agro-meteorological services, which can prolong the growing season of crops, relatively reduce the damage of frost, improve comprehensive utilization of land, and increase crop yields;at the same time, with the increase of heat resources and the northward expansion of the isoline of accumulated temperature, the area affected by pests and diseases has expanded, which has aggravated the harm to agriculture economic burden.

Characteristics of geothermal reservoirs and utilization of geothermal resources in the southeastern coastal areas of China

Based on regional geological setting, stratigraphic distribution and other geological conditions, this paper summarized three types of geothermal reservoirs in the southeast coastal areas of China: Cenozoic sandstone or sandy conglomerate reservoir, Mesozoic granite fissure reservoir and Paleozoic karst reservoir. Cenozoic sandstone or sandy conglomerate reservoirs are mainly located in Cenozoic basins, such as Zhangzhou, Fuzhou, Sanshui and Leiqiong basins. The Tertiary sedimentary basins such as Leiqiong Basin and Sanshui Basin, are controlled by NE-trending faults, while the Quaternary sedimentary such as Zhangzhou and Fuzhou basins are controlled by NW-trending faults. Mesozoic granite fissure reservoirs are mainly distributed in the southeast coastal areas, such as Zhangzhou, Fuzhou, Fengshun, Yangjiang and southern part of Hainan Province. The distribution of good Mesozoic granite fissure reservoir in these areas is mainly controlled by NE-trending faults. Paleozoic carbonate reservoirs are widely distributed in these areas. Most carbonate rocks are from the upper Paleozoic strata, such as those in the area of Huizhou in Guangdong Province. The major types of geothermal systems in the southeast coastal areas of China belong to medium and low-temperature convection. The geothermal resources developed from the ground to-3 000 m underground could be utilized directly for space heating, greenhouse heating, aquaculture pond heating and industrial uses, as well as other purposes. The geothermal resources with a depth of 3 000~6 000 m underground is mainly featured by Hot Dry Rock(HDR) with a temperature ranges from 150 ℃ to 200 ℃, which is conductive to the development of Enhanced Geothermal System(EGS) and can be utilized for power generation.

Geology and development of geothermal field in Neogene Guantao Formation in northern Bohai Bay Basin: A case of the Caofeidian geothermal heating project in Tangshan, China

Taking the Gaoshangpu-Liuzan geothermal field in the Nanpu sag of the Bohai Bay Basin as the research object, this paper discusses the geological conditions and potential of the geothermal resources of the Guantao Formation in the study area, and introduces the development practice of geothermal energy heating in Caofeidian. The average buried depth of the Guantao Formation is 1500–2500 m, the lithology is dominated by sandy conglomerate, and the average thickness of thermal reservoir is 120–300 m. The average porosity of thermal reservoir is 28%–35%, the permeability is(600–2000)×10^(-3) μm^(2), and the temperature of thermal reservoir is 70–110 ℃. The formation has total geothermal resources of 13.79×10^(18) J, equivalent to 4.70×10^(8) t of standard coal. Based on a large amount of seismic and drilling data from oil and gas exploration, this study carried out high quality target area selection, simulation of sandstone thermal reservoir, and production and injection in the same layer. The geothermal heating project with distributed production and injection well pattern covering an area of 230×10^(4) m^(2) was completed in the new district of Caofeidian in 2018. The project has been running steadily for two heating seasons, with an average annual saving of 6.06×10^(4) t of standard coal and a reduction of 15.87×10^(4) t of carbon dioxide, achieving good economic and social benefits. This project has proved that the Neogene sandstone geothermal reservoir in eastern China can achieve sustainable large-scale development by using the technology of "balanced production and injection in the same layer". It provides effective reference for the exploration and development of geothermal resource in oil and gas-bearing basins in eastern China.

Characteristics of Thermal Climate Resources Changes of Agricultural Production during Frost Period in Jianchang County

[Objective] The characteristics of thermal climate resources changes of agricultural production during frost period in Jianchang County were studied. [Method] By dint of Jianchang climate resources and routine numerical statistics method, the sunlight and temperature changes trend from 1960 to 2009 in Jianchang County were analyzed. [Result] The sunshine hours and sunshine percentages during frost period in Janchang County from 1960 to 2009 tended to decrease. The climate tendency rates were -55.556 h/10 a and -2.39%/10 a respectively, 287 h and 12% of deduction in recent 50 years. There were climate transition in 1981 and 1982. And there were a shortage of 161 h and 7% of sunshine hours and sunshine percentages before and after the transition. The temperature during the frost period generally was increasing. The average temperature, average maximum and lowest temperature tendency rate were 0.386, 0.392 and 0.567 ℃/10 a. There was a growth of 1.93, 1.96 and 2.84 ℃ in recent 50 years. There were temperature transition in 1987 and 1988. The average temperature, average maximum and lowest temperature increased 1.3, 1.2 and 1.7 ℃. In recent 50 years, the sunshine resources during frost period in Jianchang were decreasing, while the thermal resources were strengthening, forming complementary of light and heat. [Conclusion] The study provided climate accordance to the development of local facility agriculture during frost period.

Characteristics of geothermal field and evaluation of geothermal resource potential in the Yingjiang Basin

Geothermal resource,a green and sustainable energy resource,plays an important role in achieving‘emission peak’and‘carbon neutrality’targets.The Yingjiang Basin is located in the eastern branch of the Mediterranean-Himalayan high-temperature geothermal belt and exhibits considerable potential for geothermal resources.However,current investigations into the distribution of deep geothermal resources in this region are somewhat limited.In this paper,the transient plane source(TPS)method is used to measure the thermal conductivity parameters of 31 rock samples within the study area.Additionally,the one-dimensional steady-state heat conduction equation is employed to calculate the deep geothermal field,considering the constraints of rock thermal properties and terrestrial heat flow in the study area.Furthermore,the“stripping method”is used to determine the contribution rate of sedimentary layer to terrestrial heat flow,while the volume method is applied to estimate the geothermal resources at burial depths of 3000-5000 m.The results show that(1)The heat generation rate of granite is the highest with an average value of 4.52 mW/m^(3),followed by gneiss with an average value in the range of 2.0-3.5 W/(m·K),mudstone and sandstone being the lowest with an average value between 1.0 and 2.0 W/(m·K).(2)The main contributor of terrestrial heat flow in the study area is mantle heat flow,and the contribution of sedimentary layers to terrestrial heat flow only accounts for about 2%.(3)The geothermal resources in Yingjiang Basin within the depth range of 3000-5000 m is 93.6×10^(15)kJ,or 3.2×10^(9)tonnes standard coal equivalent(SCE).

Guangxi Beihai China Resources Cement Shoots at Putting into Production in May 2014

China Resources Cement in Hepu County of Beihai City is building two new type dry method cement production lines with two sets of 9 MW pure low temperatures residual heat power generating systems matched. Phase I of the project will be invested CNY I billion, and had been invested CNY 0.13 billion in 2012. China Resources Cement is shooting at putting the lines into production in May 2014.

澳洲坚果种质资源耐热性调查与分析

随着全球气候变暖,在夏季持续高温干燥天气下,我国广东、广西澳洲坚果产区不耐热的澳洲坚果种质新梢叶片出现黄化现象,直接或间接影响光合作用,进而影响产量和品质。为了筛选耐热种质应对气候变化,以位于广东省湛江市的国家热带果树种质资源(澳洲坚果)圃内的145份种质资源为试材,调查不同种质的耐热性,分析比较不同程度热敏感种质的生理特性。结果表明,湛江地区6-7月下半昼(12:00-18:00)和上半夜(18:00-24:00)经历了6次较长时间的气温高峰和湿度低谷,导致热敏感种质新梢叶片黄化。不同种质新梢叶片黄化程度因其热敏感程度不同而异,供试145份种质可划分为耐热、轻度热敏感、中度热敏感、重度热敏感种质4类。随着种质热敏感程度的加剧,叶片的叶绿素(叶绿素a+叶绿素b、叶绿素a、叶绿素b)含量均显著下降而呈现褪绿黄化;超氧阴离子自由基(O_(2)^(-))大量积累,脂氧合酶(LOX)活性显著增强,丙二醛(MDA)含量显著增加,表明由活性氧积累引发的细胞膜脂过氧化加剧。与耐热种质相比,轻度热敏感种质的超氧化物歧化酶(SOD)、过氧化物酶(POD)和过氧化氢酶(CAT)活性显著增强;随着热敏感程度加剧,中度热敏感种质和重度热敏感种质的SOD活性均显著低于耐热种质,POD活性仍显著增强,而中度热敏感种质和重度热敏感种质的CAT活性无显著性差异,表明细胞抗氧化代谢失调。

富油煤原位热解技术战略价值与科学探索

【背景】我国油气需求缺口大、供给制约多、煤炭绿色低碳转型任务艰巨,富油煤作为集煤、油、气属性于一体的煤炭资源,具有立足国内增加油气供给的巨大潜力。【进展】富油煤原位热解技术已在陕西榆林成功实施工程试验,目前仍处于探索阶段。其具备两大战略价值:一是弥补我国油气需求缺口,提高油气自主保障能力;二是变革煤炭开采技术,推动煤炭产业绿色、低碳转型发展。富油煤原位热解包括钻孔式和矿井式两种实践途径,目标是持续高效提取煤中油气资源,主要面临热解选区、加热技术与高效传热传质等难题。【展望】“四性”是原位热解技术研发的关键,包括地质条件适宜性、加热技术匹配性、传热传质有效性和热解安全稳定性。主要内容为:(1)从富油煤资源条件、地层封闭条件、水文地质条件和构造条件等方面阐明适宜富油煤原位热解的地质基础,揭示热辐射范围内围岩封闭动态稳定性的约束条件,为原位热解选址和工程设计提供地质依据。(2)深刻认识富油煤在温度、应力约束下的热物理性质演化行为,基于地质−工程条件论证原位加热技术适宜性,并针对煤层低导热特性开展高效加热工艺设计,通过风、光、电多种供能方式互补实现供热能源经济性。(3)地应力、大尺度煤体、焦油高黏度是制约原位热解油气运移、产出的主要因素,煤层致裂、载热介质优化与温压调控、焦油降黏轻质化是改善煤层传热传质性能和提高热解油气可产出性的潜在方法。(4)原位热解持续稳定运行依赖于全过程监测与动态预警,需要监测手段立体化、地质信息反演精准化、多相多场环境模型化、突变阈值预测预警等技术予以支撑。进一步探索与地质条件相匹配的富油煤原位持续高效热解关键技术,破解煤炭资源开发与地质环境之间的制约矛盾,是推动富油煤原位热解技术深入发展的关键。

水热型地热水平井取热对流传热耦合机制

【目的】闭式取热技术只利用地层热量,不抽采地热水,近年来成为地热开发研究的重点领域之一,但关注储层对流对传热影响的研究相对缺乏。【方法】为了提高单井取热量,提出水热型储层水平井闭式取热工艺,增大井筒与储层的接触面积,且充分利用储层对流。建立水平井、循环水、储层互相耦合的流动传热模型,分储层自然对流、强制对流条件开展取热性能预测,揭示储层对流场、温度场演变特征。【结果和结论】结果表明:(1)储层发育与水平段垂直的强制对流可有效缓解热突破,对取热提升较为明显;与水平段平行的强制对流与自然对流取热量无明显差异。(2)与上覆地层相比,储层段对循环水温的提升占主导地位,平均每米温度提升是上覆地层的2.4倍。(3)储层对流场和温度场演变具有高度耦合特性。当储层只存在自然对流时,温度场变化范围与达西流动活跃区局限于井筒邻近区域,沿径向方向扩展;当储层发育强制对流时,温度场和对流场在水平井筒两侧呈非对称分布,低温区和低达西流速区位于对流下游方向。(4)储层温度动态恢复特征受对流条件控制。强制对流可加速对井筒周围区域热量补给,促进温度恢复,具备长年运行的条件。研究成果为水平井取热系统研究与设计提供借鉴。

基于居里面深度对中国东北部大地热流的研究

大地热流值是表征地球热状态的重要参数,也是进行深部地温预测和评价一个地区地热资源的最基本数据。受钻孔测温的影响,盆地外的无钻孔测温地区缺少实测的大地热流值。目前的热流分布图都是依据相邻盆地的实测值进行插值绘制的,无钻孔区热流值可信度较低。由于岩石居里点与温度密切相关,可以通过居里面深度来研究地表热流值。本文依据东北地区现有的居里面深度分布图,结合实测的岩石热导率、岩石生热率数据和相应的地壳分层状况,计算了东北地区的大地热流值,重新绘制了中国东北地区精细的大地热流分布图。东北地区整体大地热流处于42.5~95 mW/m~2之间,热流高值位于五大连池及敦化-密山断裂带海龙—牡丹江一带,松辽盆地内部、小兴安岭和长春-延吉缝合带也有局部的高热流值。热流高值与居里面隆起区域有较高的一致性,即居里面隆起处热流较高,而坳陷区热流较低。本次研究填补了中国东部地区热流实测值空白,为该区深部地温预测和地热资源评价提供了更加准确的参数。

华北赋煤区地热资源富集模式及开发利用方向

【目的】中国是煤炭大国,在煤炭行业迫切需要转型的形势下,研究赋煤区的地热资源成因与分布规律十分必要。华北赋煤区地热资源储量占全国的74.7%,是中国地热资源最富集的区域之一。区内分布有渤海湾盆地、鄂尔多斯盆地、沁水盆地和南华北盆地等主要含煤盆地,其岩石圈热状态自东向西逐步降低。地热储包括新生界砂岩孔隙型和寒武-奥陶系碳酸盐岩岩溶-裂隙型两大类型。碳酸盐岩岩溶-裂隙热储温度高、水量大、易于回灌,是煤田区地热勘查与开发利用的优先选择。【方法】针对煤田区地热地质的特点,开展地热系统动力学分析,优选华北赋煤区的地热勘查与开发区域。【结果和结论】提出煤田区有以下4种聚热模式:(1)煤层与碳酸盐岩地层储盖组合传导聚热;(2)基岩面起伏变化传导聚热;(3)断裂带地下水活动对流聚热;(4)碳酸盐岩基岩面风化壳岩溶以及侵入体接触面岩溶对流聚热。并结合实例进行数值模拟分析。在此基础上,指出华北赋煤区地热勘查与开发优先方向是深部碳酸盐岩储层中的地热资源。地热能作为非碳基能源之一,以其储量大、清洁、输出连续的特点,在未来社会对电力、燃料和热力三大能源需求中的热力供应方面尤其可以做出重要贡献,而中国地热与煤炭资源在空间分布上的重叠,使地热开发利用成为煤炭行业转型的有效途径之一。

济阳坳陷深层地热资源研究进展与下步展望

济阳坳陷地热资源分布范围广、资源潜力大,是胜利油区未来地热资源开发利用的重要方向。为科学、高效地开发利用济阳坳陷地热资源,系统梳理了关于济阳坳陷水热型和干热岩型地热资源的热储层、热盖层、热源等地热地质条件,分别计算了2类地热资源的资源量,揭示其地热资源潜力。研究结果表明,济阳坳陷水热型地热资源主要赋存在馆陶组、东营组及下古生界等,其中馆陶组为水热型地热资源潜力最大的层系,分布广、资源量大,是下步重点勘探开发利用层系。济阳坳陷属于“冷壳热幔型”沉积盆地,具有较高的大地热流值,干热岩型地热资源热储层主要为太古宇的岩浆岩和变质岩,深部地幔热流是其主要热源,热储层分布面积大,温度均较高,其资源丰度为渤海湾盆地中最高。济阳坳陷地热资源丰富,为加快其开发利用步伐,建议水热型地热资源要加强地热资源与油气的关系及资源分区评价2项关键工作;干热岩型地热资源的勘探开发仍处于起步探索阶段,今后需要重点加强其热储层类型的选择与热源机制2个方面的研究。

江西芦溪县南部大地热流特征

江西省芦溪县南部地区地热资源丰富,但地热地质研究程度较低,大地热流测量工作进行的较少,制约着区域地热资源勘查开发。本文以芦溪县南部的新泉和石溪为研究区,结合钻孔岩心热物性测试和地温测井等分析了研究区岩石热导率、地温场、热源机制的特征。研究区岩石热导率平均值为2.063~6.176W/(m·K),热导率最高的为硅质石英岩,可作为良好的导热岩体。大地热流平均值为76.39 mW/m^(2),远高于中国内地地区的平均值62.5 mW/m^(2),该地区具有较高的热背景值。花岗岩放射性生热率平均值为2.16μW/m^(3),不属于高产热型岩体,放射性生热对地表热流贡献较小,热源来源为地壳深部供热。研究区构造活动强烈,深大断裂和次级断裂发育,为地下热水的深部循环提供了良好的导热和导水通道。本研究可为武功山地区的地热资源开发提供重要启示。

渤海湾盆地南堡凹陷X平台馆陶组热储潜力评价

伴随能源结构调整及“双碳”目标的推进,地热资源的勘探开发逐渐成为热点。通过地质资料整理、地温梯度计算、热储厚度解释、水质分析及采灌数值模拟等方法,探讨了渤海湾盆地南堡凹陷X平台馆陶组地热地质条件,明确了地热资源潜力。研究表明,研究区馆陶组热储岩性以砂岩为主,砂地比介于36.5%~54.9%;层顶界埋深在2 160~2 340 m,底界埋深在2 880~2 996 m,热储层有效厚度在223.4~349.6 m;热储层孔隙度介于11.4%~39.0%,渗透率平均为348.8×10^(-3)μm^(2);地层温度介于80.8~95.6℃。热储资源量为10.683×10^(18) J,折合标准煤约3.65亿t;在流量为120 m^(3)/h的采灌平衡条件下,得出地热水开采稳产30年的采灌井合理间距为400 m。研究结果为中国含油气盆地的中深层水热型地热资源勘探开采提供了有效借鉴。

中国油田地热开发利用现状与发展方向

基于中国地热发展现状、地热资源赋存和分布特点、不同地热开发方式对比,分析了油田地热资源开发利用潜力,并探讨了中国地热产业,尤其是油田地热未来的发展方向。研究结果表明:(1)中国的地热资源较为丰富,以中低温地热资源为主。浅层地热资源分布全国;中低温地热资源分布于沉积盆地、东南沿海和隆起山区,在不同深度形成了大面积分布的含地热水的热储层,为水热型地热资源;高温地热资源集中分布在西藏南部、四川西部、云南西部和台湾地区。中国浅层地热能资源(浅于200 m)年可开采量折合7×10^(8)t标准煤。(2)由于浅层地热能开发利用的环境与效率问题、深井直接换热的效率问题,以及干热岩开发利用的技术瓶颈问题,中深层水热型地热资源将是当今中国地热资源开发利用最主要和最现实的领域。(3)油田地热开发中形成了地热资源勘查与评价、砂岩地层回灌、废弃井改造为地热井、高温钻完井等一批关键技术,均在大型地热开发项目中得到成功应用。油田拥有丰富的采出水资源,可以直接利用,大量的废弃井或低效油井可以通过工艺改造为地热井进行地热资源开发,从而降低地热开发成本,提高地热项目的经济性。(4)油田地热除用于油田生产用能替代和清洁供暖外,中低温地热发电、氦气等伴生资源的开发、废弃油气藏储热和CO_(2)封存等领域的发展潜力巨大,地热综合开发利用是油田地热未来发展的主要方向。

基于单级热泵系统的再生水余热资源综合利用技术分析

当今社会环境污染与能源危机已成为全人类必须面对并要加以解决的重大课题。就采暖行业而言,人们不但需要高质量的供暖,同时还对该行业在环保、节能和安全文明生产方面提出了更高的要求。再生水源热泵技术正是满足这些要求的比较有代表性的低耗能新型供暖空调技术。以北京地区某供热中心再生水余热资源利用改造项目为例,从单级热泵技术路线出发,综合考虑以再生水余热资源为主,烟气余热、蒸汽余热为辅的3种资源形式,采用电力驱动离心式热泵设备,依托汽水换热器与热水锅炉两种调峰措施,对各种方案的技术和经济可行性进行论证和分析,最终提出安全可靠、经济高效、绿色减排、节能低碳的再生水余热资源综合利用建议。