Carbon Seq

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    Carbon Sequestration: What It Is?

    A long-term storage of carbon dioxide or other forms of carbon to either mitigate

    or defer global warming and avoid dangerous climate change.

    ore than !! billion tons of carbon emissions are noticed "annual worldwide#

    Factors to be considered-- Cost and ca$acit% of emission reduction

    - the resulting increase in demand for $rimar% energ% sources& the range of

    a$$licabilit%& and the technical ris'.

    - (ther im$ortant factors are the social and environmental consequences& the

    safet% of the technolog%& the securit% of storage and ease of monitoring and

    verification

    - )he extent of o$$ortunities to transfer the technolog% to develo$ing countries.1

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    Technological options for reducing net CO2emissions to the atmosphere

    include:

    *educing energ% consum$tion

    Switching to less carbon intensive fuels

    Increasing the use of renewable energ% sources or nuclear energ%& each of

    which emits little or no net C(+

    Sequestering C(+b% enhancing biological absor$tion ca$acit% in forests &

    soil and oceans

    Ca$turing and storing C(+chemicall% or $h%sicall%.

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    CAPTURE OF CO2

    )here are three main a$$roaches to C(+ca$ture& for industrial and $ower $lant

    a$$lications.

    ,# ost-combustion s%stems

    +# (x%-fuel combustion " still under develo$ment #

    !# re-combustion s%stems

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    ! Post-combustion captureCa$ture of C(+from flue gases $roduced b%

    combustion of fossil fuels and biomass in air.

    Instead of being discharged directl% to the

    atmos$here& flue gas is $assed through

    equi$ment which se$arates most of C(+.

    )he C(+is fed to a storage reservoir and the

    remaining flue gas is discharged to the

    atmos$here.

    A chemical sorbent $rocess would normall%

    be used for C(+se$aration.

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    2! O"#-fuel combustion captureure ox%gen is used for combustion instead

    of air& resulting in a flue gas that is mainl%C(+and +(.

    (x%gen is usuall% $roduced b% low

    tem$erature air se$aration and to su$$l%

    ox%gen to the fuel& membranes and chemicalloo$ing c%cles are being develo$ed.

    *esult -/ Almost $ure carbon dioxide

    stream can be obtained that can be

    trans$orted to the sequestration site andstored.

    )he technique is $romising& but the initial

    air se$aration ste$ demands a lot of energ%.

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    $! Pre-combustion capturere-combustion ca$ture involves reacting a fuel with ox%gen or air or steam to

    give mainl% a 0s%nthesis gas1 or 0fuel gas1 com$osed of C( and +.

    )he carbon monoxide is reacted with steam in a catal%tic reactor "shift

    converter# to give C(+and +. 6

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    %ET&O'( OF CAR)O* (E+UE(TRAT,O*

    ,. )4***4S)*IA5 S4674S)*A)I(8

    +. 94(5(9ICA5 S467AS)*A)I(8

    !. (C4A8 S4674S)*A)I(8

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    ! TERRRE(TR,A (E+UE(TRAT,O*

    )he $rocess through which C(+ from theatmos$here is absorbed naturall% through

    $hotos%nthesis stored as carbon in biomass

    soils.

    5ong-lived $lants li'e trees might 'ee$ the carbonsequestered for a long $eriod of time.

    (nce the tree dies& or as limbs& leaves& seeds& or

    blossoms dro$ from the tree& the $lant material

    decom$oses and the carbon is released.

    )ro$ical deforestation is res$onsible for +;< of

    world1s annual C(+ emissions& though offset b%

    u$ta'e of atmos$heric C(+ b% forests and

    agriculture8

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    Contd=

    Carbon seq. rates differ based on the s$ecies of tree& t%$e of soil& regionalclimate& to$ogra$h% management $ractice

    Carbon accumulation eventuall% reaches saturation $oint where additionalsequestration is no longer $ossible "when trees reach maturit%& or when theorganic matter in soils builds bac' u$ to original levels before losses

    occurred#

    After saturation& the trees or agricultural $ractices still need to be sustainedto maintain the accumulated carbon and $revent subsequent losses ofcarbon bac' to the atmos$here

    )his method is relativel% eas% to im$lement& has volume limitations. It

    might ta'e over + lac of $lants to offset the emissions from one average

    $ower $lant.

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    2 .EOO.,CA (E+UA(TRAT,O*

    It is the method of Storing C(+underground in roc' formations which are able

    to retain large amounts of C(+over a long time $eriod.

    Storage sites suggested - @eclining oil fields& saline aquifers& and

    unminable coal seams

    A / 'eclining oil fields:

    storage costs are offset b% the sale of additional oil that is recovered.

    ,;,< additional recover% of the original oil in $lace is $ossible

    C(+is soluble in oil.)he $ossible $roblems-/ lea'ages of old oil wells&

    - the high inBection $ressures and acidification which

    can damage the geological barrier.

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    ) / Unminable coal seams:

    C(+get absorbed to the coal surface& ensuring safe long-term storage.

    In the $rocess it releases methane. sale of the methane can be used to offset the cost of the C(+storage.

    c / (aline a0uifers:

    ave a large $otential storage volume and relativel% common occurrence .

    disadvantages -/

    i# As the salinit% of the water increases& less C(+can be dissolved into aqueous

    solution.

    ii# uncertaint% about the structure of a given aquifer.iii# 5ea'age of C(+bac' into the atmos$here

    owever& current research shows that several tra$$ing mechanisms immobili2e

    the C(+underground and reduces the ris' of lea'age.

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    $ OCEA* (E+UE(TRAT,O*

    Ca$tured C(+ is deliberatel% inBected into

    the ocean at great de$th& where most of itwould remain isolated from the atmos$here

    for centuries.

    C(+ can be trans$orted via $i$eline or shi$

    for release in the ocean or on the sea floor.

    (cean storage has not %et been de$lo%ed or

    thoroughl% tested.

    (ver the $ast +;; %ears the oceans have

    ta'en u$ ;; 9t C(+ from the atmos$here

    out of ,!;; 9t C(+ from total

    anthro$ogenic emissions

    Average de$th of oceans is about !;;mD

    so there is no $ractical $h%sical limit to the

    amount of C(+ that could be $laced in the

    ocean.

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    Offset .reenhouse .as Emissions

    At the global level& the ICC )hird Assessment *e$ort estimates that E,;;billion metric tons of carbon over the next ; %ears could be sequestered

    through forest $reservation& tree $lanting and im$roved agricultural

    management.

    Carbon Sequestration is not %et viable at a commercial level

    Carbon sequestration is still a develo$ing technolog%

    Concern with inBecting carbon dioxide into ground or ocean& there is fear of

    lea's into water table or esca$e of C(+ into a massive bubble that can

    $otentiall% suffocate humans and animals

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    CA(E (TU'

    Carbon se0uestration b# urban Trees on roadsides of 3adodara cit#

    F% : 9 Sandh%a Giran and Shah Ginnar% "+;,,#

    International Hournal of 4ngineering Science and )echnolog% "IH4S)# vol-!

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    Abstract

    C(+is the most significant contributor to the human influence on the greenhouse

    effect.

    )he C(+is fixed as organic carbon accumulating in the form of biomass.

    indings in re$ort suggest that J!.K tones of C(+ is removed b% trees $lanted on

    road sides of Ladodara cit% which re$resents ++< of the Cit%>s estimated total C(+$roduction.

    )otal C(+ 4mission at maBor roads was found around ,K.3J tones because of

    more number of automobiles as it is the third most-$o$ulated cit% in the Indian

    state of 9uBarat.

    *esults are restricted to the C(+that is sequestered b% trees $lanted onl% on road

    sides excluding other carbon sin's.

    It is therefore evident that tree $lanting on roadside are an effective method of

    offsetting C(+from human sources17

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    %ATER,A( A*' %ET&O'

    In this stud%& the as$ect of the measurement of the amount of carbon was

    based on the amount of standing wood% biomass of trees on the road sides ofLadodara Cit%.

    Initiall% the trees were sam$led b% quadrate method.

    6uadrates of si2e +;m x +;m were ta'en at different roadsides and at the sametime measurements of 9F "cm# and Fasal Area "m+# for different trees were

    ta'en.

    Fased on these values standing wood% biomass ")Mha# and Carbon

    sequestration rate of trees ")Mha# were calculated and then values were findout for C(+from C

    then the com$arison were done of )otal Carbon emitted and sequestered from

    all the road sites.

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    Results and discussions

    )ree cover $rovides benefits such as carbon storage and sequestration along

    with the reduction in the air $ollutant.

    So the need for evaluating and assessing the roadside tree cover in an urban

    ecos%stem becomes im$erative.

    )his green cover in the form of urban forest has a significant $otential in

    carbon sequestration.

    )he amount of carbon sequestered b% these road side trees has amounted toJ!.K tons of carbon dioxide $er %ear.

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    CO*CU(,O*(

    Cities are a maBor source of carbon dioxide emissions.

    As demonstrated b% this research $a$er urban trees $lanted on roadsides

    can hel$ in sequestering C(+ and mitigate the effects of carbon emittedfrom the automobiles.

    It is im$ortant to reduce fossil fuel emissions and $lanting large and

    health% trees to maximi2e the amount of C(+sequestered b% urban trees on

    roadsides.

    In Ladodara cit% there is need to increase roadside

    $lantation to retrieve effect of emitted carbon.

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    References

    ,. htt$:MMwww.i$cc-wg!.deMs$ecial-re$ortsMs$ecial-re$ort-on-carbon-dioxide-

    ca$ture-and-storage+. ichael ar'els& Hr and *ichard ). Farber ",3,J a% +;;,#. NSequestration

    of C(+b% ocean fertili2ationN "@#. 84)5

    !. 9 Sandh%a Giran and Shah Ginnar% "+;,,#&Ocarbon sequestration b% urban

    )rees on roadsides of Ladodara cit%O&"$df# international Bournal of engineering

    science and technolog% "IH4S)#

    3. htt$:MMwww.climatetechnolog%.gov

    . htt$:MMwww.fossil.energ%.govM$rogramsMsequestration

    P. 78CCC. Clean develo$ment mechanism "C@#. C@ $roBect search.

    *etrieved A$ril +;;

    J. Chris endri's & +;;J & 78CCC Secretariat inancial and )echnical Su$$ort

    rogramme Q Carbon Ca$ture and StorageO

    . iller& .9.& iller H.@. and Coo$er H.. ,K;.Fiomass and nutrient

    accumulation at differentgrowth rates in thinned $lantations

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    THANK YOU

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