摘要:

地热能源是一种清洁、可再生的能源,但传统的地热开发方式受到地质条件的限制,只能在少数天然渗透性好的地区进行。为了突破这一限制,科学家们提出了增强型地热系统(Enhanced Geothermal System,EGS)的概念。EGS是一种人工设计和工程化的热储层,通过化学刺激、水力压裂或热处理等技术,人为地提高储层的渗透性,从而实现对无天然渗透性地热资源的经济开采。近日,一项综合性研究对EGS领域的最新进展进行了全面评估,该研究综合了大量实验室实验、数值模拟和现场调查的结果,弥补了当前公开文献中对EGS研究成果总结不足的问题。这项研究强调了精确发育裂缝系统(无论是天然还是人工诱导的)对EGS项目成效的关键作用。值得一提的是,水力压裂技术已被证明是提高EGS性能的重要手段。与此同时,通过数值模拟开展的研究也得出了一致的结论:提高低渗透岩石的渗透性有利于EGS的高效利用。此外,该研究还指出,由于地下条件的不确定性,特别是对于处于开发初期阶段的项目,EGS的设计过程错综复杂、成本高昂。这项研究为研究人员和运营商提供了宝贵的参考,有助于提高地热能开采的效率和安全性,为未来更加可持续的EGS项目铺平了道路。EGS技术的进步不仅可以扩大地热能的开发范围,还能显著提高单位面积的发电量,降低开发成本。随着EGS技术的不断成熟,地热能有望在全球能源结构中占据更加重要的位置,为应对气候变化、实现碳中和目标做出更大贡献。不过,EGS技术的发展仍面临诸多挑战,例如如何控制储层的长期演化、如何降低诱发地震的风险等。这需要科学家、工程师和决策者的通力合作,在充分论证和严格监管的基础上稳步推进EGS项目。相信通过各方的共同努力,EGS技术定能不断突破瓶颈,为人类开启地热能利用的新纪元。对广大读者而言,这项研究无疑是一个令人振奋的好消息。它向我们展示了EGS技术的巨大潜力,以及科学家们为攻克难题所付出的艰辛努力。建议对新能源技术感兴趣的读者朋友们关注这一领域的最新动态,或许您的关注和支持,就是推动EGS技术进步的一份重要力量。让我们共同期待EGS技术的未来,期待地热能为我们带来更加清洁、高效、可靠的能源保障。同时也请记住,任何新技术的发展都需要时间和汗水,需要社会各界的理解和支持。让我们携手并进,用智慧和勇气开创人类能源利用的崭新时代!

作者|Jian Liu,Chun Shao,Baolin Yang,Mbega Ramadhani Ngata,Mathew Mwangomba,Sadock Josephat,Mohammed Dahiru Aminu

原题|Advances in enhanced geothermal systems Integrating laboratory, numerical and field insights

来源|Applied Thermal Engineering

小编|AInsightify

01

全文导读

增强型地热系统(EGS)作为一种可持续且清洁的能源,正因全球变暖导致的环境恶化而受到越来越多的关注。预计到2040年底,全球能源需求将增长25%,这主要是由人口增长和全球经济扩张所驱动的。面对当前和未来的能源需求,以及从化石燃料转向可再生能源以实现零排放目标的迫切需要,EGS被认为是一种特别有前景的可再生能源。

与常规地热系统相比,EGS通过人工优化设计,能够在没有天然地热系统的地点提取地热能。地下2-6公里深度通常存在温度超过150°C的热干岩(HDR),它们具有高温、低孔隙度和渗透率的特点,代表了一种可持续且环保的"绿色能源"。HDR的优势在于分布广泛、稳定可靠。

EGS项目的有效性在很大程度上取决于裂缝系统的精心开发,包括天然裂缝和通过水力压裂等刺激技术人工诱导的裂缝。高压冷水通过注入井注入岩石中,在深处提取热量后,热水通过生产井上升至地表,热量被利用并通过蒸汽轮机或二元电厂转化为电能。冷却后的水再次被注入地下吸收热量,形成一个闭环系统。二元循环技术在新建和在建的地热和EGS电厂中也得到广泛使用,其优势在于能够利用较低温度的资源高效运行。

Hu和Ghassemi进行了一项利用花岗岩通过EGS产生热量的实验,在水力压裂的火成岩块中循环冷水。实验结果表明,有效的裂缝面积而非总裂缝面积在控制EGS热采矿中起关键作用,这意味着需要优化注入/生产井之间的距离或生产者的位置以最大化有效换热面积。

过去40多年里,许多研究人员通过数值模拟、实验和试点测试研究EGS的开发,为EGS在能源领域的潜力和发展做出了贡献。法国、德国、澳大利亚、美国、韩国等国家都采用了EGS进行商业化利用。预计到2050年,EGS项目将在全球范围内继续增长,开发利用量将超过70GWe,届时全球已安装的地热项目将更多地集中在EGS项目上。

Hofmann等人对加拿大艾伯塔省EGS的潜力进行了全面研究,发现基底砂岩和库克湖地层作为热提取储层具有显著前景。中国南部地区如西藏、云南和东南沿海也拥有丰富的EGS资源,其潜力估计约为7.109TWhth。此外,各种数学模型已经对EGS运行期间岩层天然裂缝的行为进行了研究。

目前全球仅有少数商业EGS项目投入运营,这些项目规模较小,利用EGS技术从浅层地热资源中提取电力。其中最古老的商业EGS项目位于法国阿尔萨斯大区的苏尔兹,于1987年开始运营,装机容量为1.7MW,包括两个增强型储层,深度分别为10,000英尺和15,000英尺。许多研究表明,EGS可以在浅层和深层地层中利用。浅层EGS资源的深度低于10,000英尺,温度在30-150°C之间。位于地表以下数千英尺的深层地热资源具有巨大潜力,可产生清洁可靠的能源,尽管从枯竭井或缺乏天然流体的地区开采这些资源具有挑战性。EGS储层刺激和工程技术的发展克服了这些挑战,这些创新技术能够持续可靠地利用浅层EGS资源,从而促进了对深层EGS资源的开发。深层EGS资源可延伸至26,000英尺深,地下温度超过400°C。据AltaRock公司估计,一个100MW的地热电厂在200°C时需要40多口井,而在400°C时只需3口井,凸显了深层EGS资源在产生清洁能源方面的巨大潜力。

综上所述,EGS作为一种可持续的清洁能源,具有广阔的发展前景。通过实验室研究、数值分析和现场工作的结合,人们对EGS的认识不断深入,这有助于提高地热能开采的效率和安全性,为未来更可持续的EGS项目铺平道路。未来应继续加强研发力度,开展更多实验来深入理解岩石在高温高压下的行为,完善数值模型以准确预测储层特性,并通过现场测试和验证来评估EGS系统的实际性能。同时,还需加强全球范围内的合作与知识共享,集众家之力克服障碍,加速EGS的全球应用。政府的政策支持尤为重要,包括简化审批流程、提供财政激励措施以及制定明确的EGS实施指南,以确保环境可持续性和公共安全。最后,通过教育宣传提高公众意识,有助于消除对地热能的误解,凸显其作为清洁可再生能源的潜力。

02

HIGHLIGHT图片

Fig. 1 . EGS working mechanisms and the artificial fractures network for heat redistribution.

Fig. 2 . Five-spot system [28] .

Fig. 3 . Prediction of the exploitation of EGS globally [33] .

Fig. 4 . The locations of 18 operating and planned EGS sites worldwide [36] .

Fig. 5 . Reservoir lithology of EGS projects worldwide [64] .

Fig. 6 . EGS stimulation methods utilized worldwide [64] .

Fig. 7 . The recorded pressure data from wells during (a) low stress level fracturing tests (b) Injection and production wells (pressure history) [84] .

Fig. 8 . Secondary fractures [85] .

Fig. 10 . Schematic representation of stimulation techniques used in EGS [114] .

Fig. 11 . Bottomhole temperature for EGS projects worldwide [64] .

Fig. 12 . EGS projects with their flow rate in l/s [64] .

Fig. 13 . Flow and displacements processes (a) Numerical (b) Experiment results [138] .

Fig. 14 . Flow displacements processes (a) Numerical (b) Experiment results [138] .

Fig. 15 . Calcium carbonate scaling in geothermal wellbore and subsurface facilities [98] .

Fig. 16 . Challenges exhibited by EGS project (blue) and a successful site operation (red) [193] . (For interpretation of the references to color in this figure legend, the reader is referred to the web version of this article.)

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