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Present status and sustainable utilization of hydrothermal geothermal resources in Tianjin, China: a critical review

  • Tianjin, as one of the pioneering and most prominent cities in China, has a long history of harnessing geothermal energy. The geothermal resource available in Tianjin is primarily characterized as a low- to medium-temperature hydrothermal geothermal resource. This manuscript introduces the ongoing status and potential of geothermal utilization in China, with a particular focus on the characteristics and utilization status of geothermal resources in Tianjin, China. Moreover, the relevant strategies and challenges for cost-efficient sustainable utilization of Tianjin geothermal resources are identified. The formation parameters of heat storage characteristics of Tianjin geothermal resources are also discussed. In addition, the key paths, guidelines and challenges on how to solve the obstacles related to the geothermal resources development in Tianjin are also suggested. The summarized results indicate that the geothermal reservoirs exploited in Tianjin vary greatly, which include sandstone of Neogene Minghuazhen formation, Guantao formation, Ordovician and Cambrian and carbonate of Proterozoic Wumishan formation. Most of the exploitative geothermal resources (146 geothermal wells) in Tianjin have mainly been produced from the Wumishan formation of the Jixian system and the Guantao formation of the Neogene system. The current production capacity has been doubled, and a two-stage cascade utilization system has been established, incorporating geothermal power generation and geothermal heating. The geothermal utilization share in Tianjin is estimated to be 81.66% for heating, 16.6% for domestic hot water and 1.35% for bathing. In conclusion, notwithstanding the diversity of geothermal resources in Tianjin, it is difficult to guarantee the sustainable development and utilization of geothermal resources in Tianjin due to the unreasonable layout of geothermal wells, imbalance of production and reinjection. Hence, the integration of distributed temperature sensing and distributed strain sensing monitoring demonstrates significant promise and effectiveness in tracking water circulation and detecting flow localization problems as dynamic monitoring processes and smart thermal response tests should be recommended and established as a substantial feature required in the future utilization and development of geothermal resources in Tianjin.

    Citation: Hongmei Yin, Mohamed E Zayed, Ahmed S Menesy, Jun Zhao, Kashif Irshad, Shafiqur Rehman. Present status and sustainable utilization of hydrothermal geothermal resources in Tianjin, China: a critical review[J]. AIMS Geosciences, 2023, 9(4): 734-753. doi: 10.3934/geosci.2023039

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  • Tianjin, as one of the pioneering and most prominent cities in China, has a long history of harnessing geothermal energy. The geothermal resource available in Tianjin is primarily characterized as a low- to medium-temperature hydrothermal geothermal resource. This manuscript introduces the ongoing status and potential of geothermal utilization in China, with a particular focus on the characteristics and utilization status of geothermal resources in Tianjin, China. Moreover, the relevant strategies and challenges for cost-efficient sustainable utilization of Tianjin geothermal resources are identified. The formation parameters of heat storage characteristics of Tianjin geothermal resources are also discussed. In addition, the key paths, guidelines and challenges on how to solve the obstacles related to the geothermal resources development in Tianjin are also suggested. The summarized results indicate that the geothermal reservoirs exploited in Tianjin vary greatly, which include sandstone of Neogene Minghuazhen formation, Guantao formation, Ordovician and Cambrian and carbonate of Proterozoic Wumishan formation. Most of the exploitative geothermal resources (146 geothermal wells) in Tianjin have mainly been produced from the Wumishan formation of the Jixian system and the Guantao formation of the Neogene system. The current production capacity has been doubled, and a two-stage cascade utilization system has been established, incorporating geothermal power generation and geothermal heating. The geothermal utilization share in Tianjin is estimated to be 81.66% for heating, 16.6% for domestic hot water and 1.35% for bathing. In conclusion, notwithstanding the diversity of geothermal resources in Tianjin, it is difficult to guarantee the sustainable development and utilization of geothermal resources in Tianjin due to the unreasonable layout of geothermal wells, imbalance of production and reinjection. Hence, the integration of distributed temperature sensing and distributed strain sensing monitoring demonstrates significant promise and effectiveness in tracking water circulation and detecting flow localization problems as dynamic monitoring processes and smart thermal response tests should be recommended and established as a substantial feature required in the future utilization and development of geothermal resources in Tianjin.



    Let Fq be the finite field of q elements with characteristic p, where q=pr, p is a prime number. Let Fq=Fq{0} and Z+ denote the set of positive integers. Let sZ+ and bFq. Let f(x1,,xs) be a diagonal polynomial over Fq of the following form

    f(x1,,xs)=a1xm11+a2xm22++asxmss,

    where aiFq, miZ+, i=1,,s. Denote by Nq(f=b) the number of Fq-rational points on the affine hypersurface f=b, namely,

    Nq(f=b)=#{(x1,,xs)As(Fq)f(x1,,xs)=b}.

    In 1949, Hua and Vandiver [1] and Weil [2] independently obtained the formula of Nq(f=b) in terms of character sum as follows

    Nq(f=b)=qs1+ψ1(a11)ψs(ass)J0q(ψ1,,ψs), (1.1)

    where the sum is taken over all s multiplicative characters of Fq that satisfy ψmii=ε, ψiε, i=1,,s and ψ1ψs=ε. Here ε is the trivial multiplicative character of Fq, and J0q(ψ1,,ψs) is the Jacobi sum over Fq defined by

    J0q(ψ1,,ψs)=c1++cs=0,ciFqψ1(c1)ψs(cs).

    Though the explicit formula for Nq(f=b) are difficult to obtain in general, it has been studied extensively because of their theoretical importance as well as their applications in cryptology and coding theory; see[3,4,5,6,7,8,9]. In this paper, we use the Jacobi sums, Gauss sums and the results of quadratic form to deduce the formula of the number of Fq2-rational points on a class of hypersurfaces over Fq2 under certain conditions. The main result of this paper can be stated as

    Theorem 1.1. Let q=2r with rZ+ and Fq2 be the finite field of q2 elements. Let f(X)=a1xm11+a2xm22++asxmss, g(Y)=y1y2+y3y4++yn1yn+y2n2t1+ +y2n3+y2n1+bty2n2t++b1y2n2+b0y2n, and l(X,Y)=f(X)+g(Y), where ai,bjFq2, mi1, (mi,mk)=1, ik, mi|(q+1), miZ+, 2|n, n>2, 0tn22, TrFq2/F2(bj)=1 for i,k=1,,s and j=0,1,,t. For hFq2, we have

    (1) If h=0, then

    Nq2(l(X,Y)=0)=q2(s+n1)+γFq2(si=1((γai)mimi1)(qs+2n3+(1)tqs+n3)).

    (2) If hFq2, then

    Nq2(l(X,Y)=h)=q2(s+n1)+(qs+2n3+(1)t+1(q21)qs+n3)si=1((hai)mimi1)+γFq2{h}[si=1((γai)mimi1)(q2n+s3+(1)tqn+s3)].

    Here,

    (γai)mi={1,ifγaiisaresidueofordermi,0,otherwise.

    To prove Theorem 1.1, we need the lemmas and theorems below which are related to the Jacobi sums and Gauss sums.

    Definition 2.1. Let χ be an additive character and ψ a multiplicative character of Fq. The Gauss sum Gq(ψ,χ) in Fq is defined by

    Gq(ψ,χ)=xFqψ(x)χ(x).

    In particular, if χ is the canonical additive character, i.e., χ(x)=e2πiTrFq/Fp(x)/p where TrFq/Fp(y)=y+yp++ypr1 is the absolute trace of y from Fq to Fp, we simply write Gq(ψ):=Gq(ψ,χ).

    Let ψ be a multiplicative character of Fq which is defined for all nonzero elements of Fq. We extend the definition of ψ by setting ψ(0)=0 if ψε and ε(0)=1.

    Definition 2.2. Let ψ1,,ψs be s multiplicative characters of Fq. Then, Jq(ψ1,,ψs) is the Jacobi sum over Fq defined by

    Jq(ψ1,,ψs)=c1++cs=1,ciFqψ1(c1)ψs(cs).

    The Jacobi sums Jq(ψ1,,ψs) as well as the sums J0q(ψ1,,ψs) can be evaluated easily in case some of the multiplicative characters ψi are trivial.

    Lemma 2.3. ([10,Theorem 5.19,p. 206]) If the multiplicative characters ψ1,,ψs of Fq are trivial, then

    Jq(ψ1,,ψs)=J0q(ψ1,,ψs)=qs1.

    If some, but not all, of the ψi are trivial, then

    Jq(ψ1,,ψs)=J0q(ψ1,,ψs)=0.

    Lemma 2.4. ([10,Theorem 5.20,p. 206]) If ψ1,,ψs are multiplicative characters of Fq with ψs nontrivial, then

    J0q(ψ1,,ψs)=0

    if ψ1ψs is nontrivial and

    J0q(ψ1,,ψs)=ψs(1)(q1)Jq(ψ1,,ψs1)

    if ψ1ψs is trivial.

    If all ψi are nontrivial, there exists an important connection between Jacobi sums and Gauss sums.

    Lemma 2.5. ([10,Theorem 5.21,p. 207]) If ψ1,,ψs are nontrivial multiplicative characters of Fq and χ is a nontrivial additive character of Fq, then

    Jq(ψ1,,ψs)=Gq(ψ1,χ)Gq(ψs,χ)Gq(ψ1ψs,χ)

    if ψ1ψs is nontrivial and

    Jq(ψ1,,ψs)=ψs(1)Jq(ψ1,,ψs1)=1qGq(ψ1,χ)Gq(ψs,χ)

    if ψ1ψs is trivial.

    We turn to another special formula for Gauss sums which applies to a wider range of multiplicative characters but needs a restriction on the underlying field.

    Lemma 2.6. ([10,Theorem 5.16,p. 202]) Let q be a prime power, let ψ be a nontrivial multiplicative character of Fq2 of order m dividing q+1. Then

    Gq2(ψ)={q,ifmoddorq+1meven,q,ifmevenandq+1modd.

    For hFq2, define v(h)=1 if hFq2 and v(0)=q21. The property of the function v(h) will be used in the later proofs.

    Lemma 2.7. ([10,Lemma 6.23,p. 281]) For any finite field Fq, we have

    cFqv(c)=0,

    for any bFq,

    c1++cm=bv(c1)v(ck)={0,1k<m,v(b)qm1,k=m,

    where the sum is over all c1,,cmFq with c1++cm=b.

    The quadratic forms have been studied intensively. A quadratic form f in n indeterminates is called nondegenerate if f is not equivalent to a quadratic form in fewer than n indeterminates. For any finite field Fq, two quadratic forms f and g over Fq are called equivalent if f can be transformed into g by means of a nonsingular linear substitution of indeterminates.

    Lemma 2.8. ([10,Theorem 6.30,p. 287]) Let fFq[x1,,xn], q even, be a nondegenerate quadratic form. If n is even, then f is either equivalent to

    x1x2+x3x4++xn1xn

    or to a quadratic form of the type

    x1x2+x3x4++xn1xn+x2n1+ax2n,

    where aFq satisfies TrFq/Fp(a)=1.

    Lemma 2.9. ([10,Corollary 3.79,p. 127]) Let aFq and let p be the characteristic of Fq, the trinomial xpxa is irreducible in Fq if and only if TrFq/Fp(a)0.

    Lemma 2.10. ([10,Lemma 6.31,p. 288]) For even q, let aFq with TrFq/Fp(a)=1 and bFq. Then

    Nq(x21+x1x2+ax22=b)=qv(b).

    Lemma 2.11. ([10,Theorem 6.32,p. 288]) Let Fq be a finite field with q even and let bFq. Then for even n, the number of solutions of the equation

    x1x2+x3x4++xn1xn=b

    in Fnq is qn1+v(b)q(n2)/2. For even n and aFq with TrFq/Fp(a)=1, the number of solutions of the equation

    x1x2+x3x4++xn1xn+x2n1+ax2n=b

    in Fnq is qn1v(b)q(n2)/2.

    Lemma 2.12. Let q=2r and hFq2. Let g(Y)Fq2[y1,y2,,yn] be a polynomial of the form

    g(Y)=y1y2+y3y4++yn1yn+y2n2t1++y2n3+y2n1+bty2n2t++b1y2n2+b0y2n,

    where bjFq2, 2|n, n>2, 0tn22, TrFq2/F2(bj)=1, j=0,1,,t. Then

    Nq2(g(Y)=h)=q2(n1)+(1)t+1qn2v(h). (2.1)

    Proof. We provide two proofs here. The first proof is as follows. Let q1=q2. Then by Lemmas 2.7 and 2.10, the number of solutions of g(Y)=h in Fq2 can be deduced as

    Nq2(g(Y)=h)=c1+c2++ct+2=hNq2(y1y2+y3y4++yn2t3yn2t2=c1)Nq2(yn2t1yn2t+y2n2t1+bty2n2t=c2)Nq2(yn1yn+y2n1+b0y2n=ct+2)=c1+c2++ct+2=h(qn2t31+v(c1)q(n2t4)/21)(q1v(c2))(q1v(ct+2))=c1+c2++ct+2=h(qn2t21+v(c1)q(n2t2)/21v(c2)qn2t31v(c1)v(c2)q(n2t4)/21)(q1v(c3))(q1v(ct+2))=c1+c2++ct+2=h(qnt21+v(c1)q(n2)/21v(c2)qnt31++(1)t+1v(c1)v(c2)v(ct+2)q(n2t4)/21)=qn11+q(n2)/21c1Fq2v(c1)++(1)t+1c1+c2++ct+2=hv(c1)v(c2)v(ct+2)q(n2t4)/21. (2.2)

    By Lamma 2.7 and (2.2), we have

    Nq2(g(Y)=h)=qn11+(1)t+1v(h)q(n2)/21=q2(n1)+(1)t+1v(h)qn2.

    Next we give the second proof. Note that if f and g are equivalent, then for any bFq2 the equation f(x1,,xn)=b and g(x1,,xn)=b have the same number of solutions in Fq2. So we can get the number of solutions of g(Y)=h for hFq2 by means of a nonsingular linear substitution of indeterminates.

    Let k(X)Fq2[x1,x2,x3,x4] and k(X)=x1x2+x21+Ax22+x3x4+x23+Bx24, where TrFq2/F2(A)=TrFq2/F2(B)=1. We first show that k(x) is equivalent to x1x2+x3x4.

    Let x3=y1+y3 and xi=yi for i3, then k(X) is equivalent to y1y2+y1y4+y3y4+Ay22+y23+By24.

    Let y2=z2+z4 and yi=zi for i2, then k(X) is equivalent to z1z2+z3z4+Az22+z23+Az24+Bz24.

    Let z1=α1+Aα2 and zi=αi for i1, then k(X) is equivalent to α1α2+α23+α3α4+(A+B)α24.

    Since TrFq2/F2(A+B)=0, we have α23+α3α4+(A+B)α24 is reducible by Lemma 2.9. Then k(X) is equivalent to x1x2+x3x4. It follows that if t is odd, then g(Y) is equivalent to x1x2+x3x4++xn1xn, and if t is even, then g(Y) is equivalent to x1x2+x3x4++xn1xn+x2n1+ax2n with TrFq2/F2(a)=1. By Lemma 2.11, we get the desired result.

    From (1.1), we know that the formula for the number of solutions of f(X)=0 over Fq2 is

    Nq2(f(X)=0)=q2(s1)+d11j1=1ds1js=1¯ψj11(a1)¯ψjss(as)J0q2(ψj11,,ψjss),

    where di=(mi,q21) and ψi is a multiplicative character of Fq2 of order di. Since mi|q+1, we have di=mi. Let H={(j1,,js)1ji<mi, 1is}. It follows that ψj11ψjss is nontrivial for any (j1,,js)H as (mi,mj)=1. By Lemma 2, we have J0q2(ψj11,,ψjss)=0 and hence Nq2(f(X)=0)=q2(s1).

    Let Nq2(f(X)=c) denote the number of solutions of the equation f(X)=c over Fq2 with cFq2. Let V={(j1,,js)|0ji<mi,1is}. Then

    Nq2(f(X)=c)=γ1++γs=cNq2(a1xm11=γ1)Nq2(asxmss=γs)=γ1++γs=cm11j1=0ψj11(γ1a1)ms1js=0ψjss(γsas).

    Since ψi is a multiplicative character of Fq2 of order mi, we have

    Nq2(f(X)=c)=γ1c++γsc=1(j1,,js)Vψj11(γ1c)ψj11(ca1)ψjss(γsc)ψjss(cas)=(j1,,js)Vψj11(ca1)ψjss(cas)γ1c++γsc=1ψj11(γ1c)ψjss(γsc)=(j1,,js)Vψj11(ca1)ψjss(cas)Jq2(ψj11,,ψjss).

    By Lemma 2.3,

    Nq2(f(X)=c)=q2(s1)+(j1,,js)Hψj11(ca1)ψjss(cas)Jq2(ψj11,,ψjss).

    By Lemma 2.5,

    Jq2(ψj11,,ψjss)=Gq2(ψj11)Gq2(ψjss)Gq2(ψj11ψjss).

    Since mi|q+1 and 2mi, by Lemma 2.6, we have

    Gq2(ψj11)==Gq2(ψjss)=Gq2(ψj11ψjss)=q.

    Then

    Nq2(f(X)=c)=q2(s1)+qs1m11j1=1ψj11(ca1)ms1js=1ψjss(cas)=q2(s1)+qs1(m11j1=0ψj11(ca1)1)(ms1js=0ψjss(cas)1).

    It follows that

    Nq2(f(X)=c)=q2(s1)+qs1si=1((cai)mimi1), (3.1)

    where

    (cai)mi={1,ifcai is a residue of ordermi,0,otherwise.

    For a given hFq2. We discuss the two cases according to whether h is zero or not.

    Case 1: h=0. If f(X)=0, then g(Y)=0; if f(X)0, then g(Y)0. Then

    Nq2(l(X,Y)=0)=c1+c2=0Nq2(f(X)=c1)Nq2(g(Y)=c2)=q2(s1)(q2(n1)+(1)t+1(q21)qn2)+c1+c2=0c1,c2Fq2Nq2(f(X)=c1)Nq2(g(Y)=c2). (3.2)

    By Lemma 2.12, (3.1) and (3.2), we have

    Nq2(l(X,Y)=0)=q2(s+n2)+(1)t+1q2(s1)+hn(1)t+1q2(s2)+n+c1Fq2[q2(s+n2)(1)t+1q2(s2)+n+si=1((c1ai)mimi1)(q2n+s3(1)t+1qn+s3)]=q2(s+n2)+(1)t+1q2(s1)+n(1)t+1q2(s2)+n+q2(s+n1)(1)t+1q2(s1)+nq2(s+n2)+(1)t+1q2(s2)+n+c1Fq2[si=1((c1ai)mimi1)(q2n+s3(1)t+1qn+s3)]=q2(s+n1)+c1Fq2[si=1((c1ai)mimi1)(q2n+s3(1)t+1qn+s3)]. (3.3)

    Case 2: hFq2. If f(X)=h, then g(Y)=0; if f(X)=0, then g(Y)=h; if f(X){0,h}, then g(Y){0,h}. So we have

    Nq2(l(X,Y))=h)=c1+c2=hNq2(f(X)=c1)Nq2(g(Y)=c2)=Nq2(f(X)=0)Nq2(g(Y)=h)+Nq2(f(X)=h)Nq2(g(Y)=0)+c1+c2=hc1,c2Fq2{h}Nq2(f(X)=c1)Nq2(g(Y)=c2). (3.4)

    By Lemma 2.12, (3.1) and (3.4),

    Nq2(l(X,Y)=h)=2q2(s+n2)+(1)t+1q2s+n2(1)t+12q2s+n4+(qs+2n3+(1)t+1(q21)qs+n3)si=1((hai)mimi1)+c1Fq2{h}[q2(s+n2)(1)t+1q2s+n4+si=1((c1ai)mimi1)(q2n+s3(1)t+1qn+s3)].

    It follows that

    Nq2(l(X,Y)=h)=2q2(s+n2)+(1)t+1q2s+n2(1)t+12q2s+n4+(qs+2n3+(1)t+1(q21)qs+n3)si=1((hai)mimi1)+c1Fq2{h}[q2(s+n2)(1)t+1q2s+n4+si=1((c1ai)mimi1)(q2n+s3(1)t+1qn+s3)]=q2(s+n1)+(qs+2n3+(1)t+1(q21)qs+n3)si=1((hai)mimi1)+c1Fq2{h}[si=1((c1ai)mimi1)(q2n+s3+(1)tqn+s3)]. (3.5)

    By (3.3) and (3.5), we get the desired result. The proof of Theorem 1.1 is complete.

    There is a direct corollary of Theorem 1.1 and we omit its proof.

    Corollary 4.1. Under the conditions of Theorem 1.1, if a1==as=hFq2, then we have

    Nq2(l(X,Y)=h)=q2(s+n1)+(qs+2n3+(1)t+1(q21)qs+n3)si=1(mi1)+γFq2{h}[si=1((γh)mimi1)(q2n+s3+(1)tqn+s3)],

    where

    (γh)mi={1,ifγhisaresidueofordermi,0,otherwise.

    Finally, we give two examples to conclude the paper.

    Example 4.2. Let F210=α=F2[x]/(x10+x3+1) where α is a root of x10+x3+1. Suppose l(X,Y)=α33x31+x112+y23+α10y24+y1y2+y3y4. Clearly, TrF210/F2(α10)=1, m1=3, m2=11, s=2, n=4, t=0, a2=1. By Theorem 1.1, we have

    N210(l(X,Y)=0)=10245+(327+323)×20=1126587102265344.

    Example 4.3. Let F212=β=F2[x]/(x12+x6+x4+x+1) where β is a root of x12+x6+x4+x+1. Suppose l(X,Y)=x51+x132+y23+β10y24+y1y2+y3y4. Clearly, TrF212/F2(β10)=1, m1=5, m2=13, s=2, n=4, t=0, a1=a2=1. By Corollary 1, we have

    N212(l(X,Y)=1)=25×12+(647643×4095)×48=1153132559312355328.

    This work was jointly supported by the Natural Science Foundation of Fujian Province, China under Grant No. 2022J02046, Fujian Key Laboratory of Granular Computing and Applications (Minnan Normal University), Institute of Meteorological Big Data-Digital Fujian and Fujian Key Laboratory of Data Science and Statistics.

    The authors declare there is no conflicts of interest.



    [1] El-Hadary MI, Senthilraja S, Zayed ME (2023) A hybrid system coupling spiral type solar photovoltaic thermal collector and electrocatalytic hydrogen production cell: Experimental investigation and numerical modeling. Process Saf Environ Prot 170: 1101–1120. https://doi.org/10.1016/j.psep.2022.12.079 doi: 10.1016/j.psep.2022.12.079
    [2] Zayed ME, Zhao J, Li W, et al. (2020) Recent progress in phase change materials storage containers: Geometries, design considerations and heat transfer improvement methods. J Energy Storage 30: 101341. https://doi.org/10.1016/j.est.2020.101341 doi: 10.1016/j.est.2020.101341
    [3] Zayed ME, Zhao J, Elsheikh AH, et al. (2021) A comprehensive review on Dish/Stirling concentrated solar power systems: Design, optical and geometrical analyses, thermal performance assessment, and applications. J Clean Prod 283: 124664. https://doi.org/10.1016/j.jclepro.2020.124664 doi: 10.1016/j.jclepro.2020.124664
    [4] Zhao J, Ma L, Zayed ME, et al. (2021) Industrial reheating furnaces: A review of energy efficiency assessments, waste heat recovery potentials, heating process characteristics and perspectives for steel industry. Process Saf Environ Prot 147: 1209–1228. https://doi.org/10.1016/j.psep.2021.01.045 doi: 10.1016/j.psep.2021.01.045
    [5] Zayed ME, Zhao J, Elsheikh AH, et al. (2020) Optimal design parameters and performance optimization of thermodynamically balanced dish/Stirling concentrated solar power system using multi-objective particle swarm optimization. Appl Therm Eng 178: 115539. https://doi.org/10.1016/j.applthermaleng.2020.115539 doi: 10.1016/j.applthermaleng.2020.115539
    [6] Aboelmaaref MM, Zayed ME, Zhao J, et al. (2020) Hybrid solar desalination systems driven by parabolic trough and parabolic dish CSP technologies: Technology categorization, thermodynamic performance and economical assessment. Energy Convers Manag 220: 113103. https://doi.org/10.1016/j.enconman.2020.113103 doi: 10.1016/j.enconman.2020.113103
    [7] Ma L, Li Y, Wang JY, et al. (2019) A thermal-dissipation correction method for in-situ soil thermal response test: Experiment and simulation under multi-operation conditions. Energy Build 194: 218–231. https://doi.org/10.1016/j.enbuild.2019.04.014 doi: 10.1016/j.enbuild.2019.04.014
    [8] Al-Kbodi BH, Rajeh T, Li Y, et al. (2023) Heat extraction analyses and energy consumption characteristics of novel designs of geothermal borehole heat exchangers with elliptic and oval double U-tube structures. Appl Therm Eng 235: 121418. https://doi.org/10.1016/j.applthermaleng.2023.121418 doi: 10.1016/j.applthermaleng.2023.121418
    [9] Nian YL, Cheng WL (2018) Insights into geothermal utilization of abandoned oil and gas wells. Renewable Sustainable Energy Rev 87: 44–60. https://doi.org/10.1016/j.rser.2018.02.004 doi: 10.1016/j.rser.2018.02.004
    [10] Kamazani M, Aghanajafi C (2022) Numerical simulation of geothermal-PVT hybrid system with PCM storage tank. Int J Energy Res 46: 397–414. https://doi.org/10.1002/er.7279 doi: 10.1002/er.7279
    [11] Ma L, Zhao Y, Yin HM, et al. (2019) A coupled heat transfer model of medium-depth downhole coaxial heat exchanger based on the piecewise analytical solution. Energy Convers Manage 204: 112308. https://doi.org/10.1016/j.enconman.2019.112308 doi: 10.1016/j.enconman.2019.112308
    [12] Gilbert GL, Instanes A, Sinitsyn AO, et al. (2019) Characterization of two sites for geotechnical testing in permafrost: Longyearbyen, Svalbard. AIMS Geosci 5: 868–885. https://doi.org/10.3934/geosci.2019.4.868 doi: 10.3934/geosci.2019.4.868
    [13] Marmelia PD, Andri DS, Yusuf L (2022) Investment decisions under uncertainties in geothermal power generation. AIMS Energy 4: 844–857. https://doi.org/10.3934/energy.2022038 doi: 10.3934/energy.2022038
    [14] Kelly JJ, McDermott CI (2022) Numerical modelling of a deep closed-loop geothermal system: evaluating the Eavor-Loop. AIMS Geosci 8: 175–212. https://doi.org/10.3934/geosci.2022011 doi: 10.3934/geosci.2022011
    [15] Zayed ME, Shboul B, Yin H, et al. (2022) Recent advances in geothermal energy reservoirs modeling: Challenges and potential of thermo-fluid integrated models for reservoir heat extraction and geothermal energy piles design. J Energy Storage 62: 106835. https://doi.org/10.1016/j.est.2023.106835 doi: 10.1016/j.est.2023.106835
    [16] Su Y, Yang F, Wang B, et al. (2018) Reinjection of cooled water into sandstone geothermal reservoirs in China: a review. Geosci J 22: 199–207. https://doi.org/10.1007/s12303-017-0019-3 doi: 10.1007/s12303-017-0019-3
    [17] Song W, Liu X, Zheng T, et al. (2020) A review of recharge and clogging in sandstone aquifer. Geothermics 87: 101857. https://doi.org/10.1016/j.geothermics.2020.101857 doi: 10.1016/j.geothermics.2020.101857
    [18] Dijkshoorn L, Speer S, Pechnig R (2013) Measurements and design calculations for a deep coaxial borehole heat exchanger in Aachen, Germany. Int J Geophys 2013: 916541. https://doi.org/10.1155/2013/916541 doi: 10.1155/2013/916541
    [19] Wu BS, Zhang X, Jeffrey RG, et al. (2016) A simplified model for heat extraction by circulating fluid through a closed-loop multiple-fracture enhanced geothermal system. Appl Energy 183: 1664–1681. https://doi.org/10.1016/j.apenergy.2016.09.113 doi: 10.1016/j.apenergy.2016.09.113
    [20] Willems CJL, Nick HM, Weltje GJ, et al. (2017) An evaluation of interferences in heat production from low enthalpy geothermal doublets systems. Energy 135: 500–512. https://doi.org/10.1016/j.energy.2017.06.129 doi: 10.1016/j.energy.2017.06.129
    [21] Lund JW, Boyd TL (2016) Direct utilization of geothermal energy worldwide: review. Geothermics 60: 66–93. https://doi.org/10.1016/j.geothermics.2015.11.004 doi: 10.1016/j.geothermics.2015.11.004
    [22] Babaei M, Nick HM (2019) Performance of low-enthalpy geothermal systems: interplay of spatially correlated heterogeneity and well-doublet spacings. Appl Energy 253: 113569. https://doi.org/10.1016/j.apenergy.2019.113569 doi: 10.1016/j.apenergy.2019.113569
    [23] Holmberg H, Acuña J, Næss E, et al. (2016) Thermal evaluation of coaxial deep borehole heat exchangers. Renew Energy 97: 65–76. https://doi.org/10.1016/j.renene.2016.05.048 doi: 10.1016/j.renene.2016.05.048
    [24] Liu H, Hou Z, Li X, et al. (2015) A preliminary site selection system for a CO2-AGES project and its application in China. Environ Earth Sci 73: 6855–6870. https://doi.org/10.1007/s12665-015-4249-2 doi: 10.1007/s12665-015-4249-2
    [25] Zhu JL, Hu K, Lu X, et al. (2015) A review of geothermal energy resources, development, and applications in China: Current status and prospects. Energy 93: 466–483. https://doi.org/10.1016/j.energy.2015.08.098 doi: 10.1016/j.energy.2015.08.098
    [26] An QS, Wang YZ, Zhao J, et al. (2016) Direct utilization status and power generation potential of low-medium temperature hydrothermal geothermal resources in Tianjin, China: A review. Geothermics 64: 426–438. https://doi.org/10.1016/j.geothermics.2016.06.005 doi: 10.1016/j.geothermics.2016.06.005
    [27] Wang YZ, Li CJ, Zhao J, et al. (2021) The above-ground strategies to approach the goal of geothermal power generation in China: State of art and future researches. Renewable Sustainable Energy Rev 138: 110557. https://doi.org/10.1016/j.rser.2020.110557 doi: 10.1016/j.rser.2020.110557
    [28] Zhang L, Chen S, Zhang C (2019) Geothermal power generation in China: Status and prospects. Energy Sci Eng 7: 1428–1450. https://doi.org/10.1002/ese3.365 doi: 10.1002/ese3.365
    [29] Xu YS, Wang XW, Shen SL, et al. (2020) Distribution characteristics and utilization of shallow geothermal energy in China. Energy Build 229: 110479. https://doi.org/10.1016/j.enbuild.2020.110479 doi: 10.1016/j.enbuild.2020.110479
    [30] He Z, Feng J, Luo J, et al. (2023) Distribution, exploitation, and utilization of intermediate-to-deep geothermal resources in eastern China. Energy Geosci 4: 100187. https://doi.org/10.1016/j.engeos.2023.100187 doi: 10.1016/j.engeos.2023.100187
    [31] Luo J, Zhang Q, Liang C, et al. (2023) An overview of the recent development of the Ground Source Heat Pump (GSHP) system in China, Renew. Energy 210: 269–279. https://doi.org/https://doi.org/10.1016/j.renene.2023.04.034 doi: 10.1016/j.renene.2023.04.034
    [32] Duan YH, Wang JB, Wang YB, et al. (2004) Groundwater resources and its sustainable development in Tianjin. Hydrol Eng Geol 31: 29–39.
    [33] Zhang WK, Wang KX, Guan CM, et al. (2023) Analysis and optimization of the performance for the ground source heat pump system with the middle-deep U-type well. Appl Therm Eng 219: 119404. https://doi.org/10.1016/j.applthermaleng.2022.119404 doi: 10.1016/j.applthermaleng.2022.119404
    [34] Tian P (2015) Evaluation on the Potential of Geothermal Resource in Tianjin. China University of Geosciences, Thesis.
    [35] Yu Y (2014) Evaluation of geothermal resources in the Neogene geothermal reservoir in the New Coastal Area of Tianjin. China University of Geosciences, Thesis.
    [36] Lei HY, Zhu JL (2013) Numerical modeling of exploitation and reinjection of the Guantao geothermal reservoir in Tanggu District, Tianjin, China. Geothermics 48: 60–68. https://doi.org/10.1016/j.geothermics.2013.03.008 doi: 10.1016/j.geothermics.2013.03.008
    [37] Rajeh T, Al-Kbodi BH, Li Y, et al. (2023) Modeling and techno-economic comparison of two types of coaxial with double U-tube ground heat exchangers. Appl Therm Eng 225: 120221. https://doi.org/10.1016/j.applthermaleng.2023.120221 doi: 10.1016/j.applthermaleng.2023.120221
    [38] Qian H (2014) Study of the feasibility of geothermal well drilling technology in the Cambrian in the Dongli District of Tianjin. China University of Geosciences. A thesis.
    [39] Parisio F, Yoshioka K (2020) Modeling fluid reinjection into an enhanced geothermal system. Geophys Res Lett 47. https://doi.org/10.1029/2020GL089886 doi: 10.1029/2020GL089886
    [40] Ke TT, Huang SP, Xu W, et al. (2022) Evaluation of the multi-doublet performance in sandstone reservoirs using thermal-hydraulic modeling and economic analysis. Geothermics 98: 102273. https://doi.org/10.1016/j.geothermics.2021.102273 doi: 10.1016/j.geothermics.2021.102273
    [41] Rajeh T, Al-Kbodi BH, Li Y, et al. (2023) A novel oval-shaped coaxial ground heat exchanger for augmenting the performance of ground-coupled heat pumps: Transient heat transfer performance and multi-parameter optimization. J Build Eng 79: 107781. https://doi.org/10.1016/j.jobe.2023.107781 doi: 10.1016/j.jobe.2023.107781
    [42] Wang GL, Wang WL, Zhang W, et al. (2020) The status quo and prospect of geothermal resources exploration and development in Beijing-Tianj in-Hebei region in China. China Geol 3: 173–181. https://doi.org/10.31035/cg2020013 doi: 10.31035/cg2020013
    [43] Wang Y, Liu Y, Dou J, et al. (2020) Geothermal energy in China: Status, challenges, and policy recommendations. Utilities Policy 64: 101020. https://doi.org/10.1016/j.jup.2020.101020 doi: 10.1016/j.jup.2020.101020
    [44] Wang L, Bi Y, Yao J, et al. (2022) Comprehensive Utilization of Resources, Interpretation of Green Mine Evaluation Index, Springer, Singapore. https://doi.org/10.1007/978-981-16-5433-6_6
    [45] Jian Z, Gui F, Yubei H (2023) The deep high temperature characteristics and geodynamic background of geothermal anomaly areas in Eastern China. Earth Sci Front 30: 316–332.
    [46] Bing MR, Jia LX, Yang Y, et al. (2021) The development and utilization of geothermal energy in the world. Chin Geol 48: 1734–1747. https://doi.org/10.12029/gc20210606 doi: 10.12029/gc20210606
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