An issue of permanence: Assessing the effectiveness of temporary carbon storage

被引:113
作者
Herzog, H
Caldeira, K
Reilly, J
机构
[1] MIT, Lab Energy & Environm, Cambridge, MA 02139 USA
[2] Lawrence Livermore Natl Lab, Livermore, CA 94550 USA
[3] MIT, Joint Program Sci & Policy Global Change, Cambridge, MA 02139 USA
关键词
D O I
10.1023/A:1024801618900
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this paper, we present a method to quantify the effectiveness of carbon mitigation options taking into account the 'permanence' of the emissions reduction. While the issue of permanence is most commonly associated with a 'leaky' carbon sequestration reservoir, we argue that this is an issue that applies to just about all carbon mitigation options. The appropriate formulation of this problem is to ask 'what is the value of temporary storage?' Valuing temporary storage can be represented as a familiar economic problem, with explicitly stated assumptions about carbon prices and the discount rate. To illustrate the methodology, we calculate the sequestration effectiveness for injecting CO2 at various depths in the ocean. Analysis is performed for three limiting carbon price assumptions: constant carbon prices ( assumes constant marginal damages), carbon prices rise at the discount rate ( assumes efficient allocation of a cumulative emissions cap without a backstop technology), and carbon prices first rise at the discount rate but become constant after a given time ( assumes introduction of a backstop technology). Our results show that the value of relatively deep ocean carbon sequestration can be nearly equivalent to permanent sequestration if marginal damages ( i.e., carbon prices) remain constant or if there is a backstop technology that caps the abatement cost in the not too distant future. On the other hand, if climate damages are such as to require a fixed cumulative emissions limit and there is no backstop, then a storage option with even very slow leakage has limited value relative to a permanent storage option.
引用
收藏
页码:293 / 310
页数:18
相关论文
共 38 条
[1]  
[Anonymous], DOESCFE1
[2]  
[Anonymous], ENERGY J
[3]   SOURCES AND FLOW PATTERNS OF DEEP-OCEAN WATERS AS DEDUCED FROM POTENTIAL TEMPERATURE, SALINITY, AND INITIAL PHOSPHATE CONCENTRATION [J].
BROECKER, WS ;
TAKAHASHI, T ;
TAKAHASHI, T .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1985, 90 (NC4) :6925-6939
[4]   OCEANIC RADIOCARBON - SEPARATION OF THE NATURAL AND BOMB COMPONENTS [J].
BROECKER, WS ;
SUTHERLAND, S ;
SMETHIE, W ;
PENG, TH ;
OSTLUND, G .
GLOBAL BIOGEOCHEMICAL CYCLES, 1995, 9 (02) :263-288
[5]   Predicted net efflux of radiocarbon from the ocean and increase in atmospheric radiocarbon content [J].
Caldeira, K ;
Rau, GH ;
Duffy, PB .
GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (20) :3811-3814
[6]  
CALDEIRA K, 2002, GEOPHYS RES LETT, V8
[7]  
CALDEIRA K, 2001, P 1 NAT C CARB SEQ W
[8]   THERMODYNAMICS OF THE DISSOCIATION OF BORIC-ACID IN SYNTHETIC SEAWATER FROM 273.15-K TO 318.15-K [J].
DICKSON, AG .
DEEP-SEA RESEARCH PART A-OCEANOGRAPHIC RESEARCH PAPERS, 1990, 37 (05) :755-766
[9]  
DUBEY MK, 2002, ACS DIVISION FUEL CH, V47, P81
[10]  
EDMONDS JA, 1995, MODELING GLOBAL CHAN, P295