CA2853638A1 - Process and methodology for quantifying carbon offsets from ocean phytoplankton stimulation - Google Patents
Process and methodology for quantifying carbon offsets from ocean phytoplankton stimulation Download PDFInfo
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- CA2853638A1 CA2853638A1 CA2853638A CA2853638A CA2853638A1 CA 2853638 A1 CA2853638 A1 CA 2853638A1 CA 2853638 A CA2853638 A CA 2853638A CA 2853638 A CA2853638 A CA 2853638A CA 2853638 A1 CA2853638 A1 CA 2853638A1
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- chlorophyll
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- 238000000034 method Methods 0.000 title claims abstract description 19
- OKTJSMMVPCPJKN-UHFFFAOYSA-N Carbon Chemical compound [C] OKTJSMMVPCPJKN-UHFFFAOYSA-N 0.000 title claims abstract description 16
- 229910052799 carbon Inorganic materials 0.000 title claims abstract description 16
- 230000000638 stimulation Effects 0.000 title claims description 3
- ATNHDLDRLWWWCB-AENOIHSZSA-M chlorophyll a Chemical compound C1([C@@H](C(=O)OC)C(=O)C2=C3C)=C2N2C3=CC(C(CC)=C3C)=[N+]4C3=CC3=C(C=C)C(C)=C5N3[Mg-2]42[N+]2=C1[C@@H](CCC(=O)OC\C=C(/C)CCC[C@H](C)CCC[C@H](C)CCCC(C)C)[C@H](C)C2=C5 ATNHDLDRLWWWCB-AENOIHSZSA-M 0.000 claims abstract description 14
- 229930002875 chlorophyll Natural products 0.000 claims abstract description 12
- 235000019804 chlorophyll Nutrition 0.000 claims abstract description 12
- 238000006243 chemical reaction Methods 0.000 claims abstract description 3
- CURLTUGMZLYLDI-UHFFFAOYSA-N Carbon dioxide Chemical compound O=C=O CURLTUGMZLYLDI-UHFFFAOYSA-N 0.000 claims abstract 12
- XEEYBQQBJWHFJM-UHFFFAOYSA-N Iron Chemical compound [Fe] XEEYBQQBJWHFJM-UHFFFAOYSA-N 0.000 claims abstract 10
- 229910002092 carbon dioxide Inorganic materials 0.000 claims abstract 6
- 239000001569 carbon dioxide Substances 0.000 claims abstract 6
- 229910052742 iron Inorganic materials 0.000 claims abstract 5
- 235000015097 nutrients Nutrition 0.000 claims abstract 2
- 230000000243 photosynthetic effect Effects 0.000 claims abstract 2
- 230000009919 sequestration Effects 0.000 claims description 9
- 238000005259 measurement Methods 0.000 claims description 4
- 230000007613 environmental effect Effects 0.000 claims description 2
- 150000002506 iron compounds Chemical class 0.000 claims 4
- 229930002868 chlorophyll a Natural products 0.000 claims 2
- XLYOFNOQVPJJNP-UHFFFAOYSA-N water Substances O XLYOFNOQVPJJNP-UHFFFAOYSA-N 0.000 claims 1
- 239000011785 micronutrient Substances 0.000 abstract 2
- 235000013369 micronutrients Nutrition 0.000 abstract 2
- WQZGKKKJIJFFOK-GASJEMHNSA-N Glucose Natural products OC[C@H]1OC(O)[C@H](O)[C@@H](O)[C@@H]1O WQZGKKKJIJFFOK-GASJEMHNSA-N 0.000 abstract 1
- QVGXLLKOCUKJST-UHFFFAOYSA-N atomic oxygen Chemical compound [O] QVGXLLKOCUKJST-UHFFFAOYSA-N 0.000 abstract 1
- 230000002950 deficient Effects 0.000 abstract 1
- 239000007789 gas Substances 0.000 abstract 1
- 239000008103 glucose Substances 0.000 abstract 1
- 229910052760 oxygen Inorganic materials 0.000 abstract 1
- 239000001301 oxygen Substances 0.000 abstract 1
- 230000004936 stimulating effect Effects 0.000 abstract 1
- 239000000126 substance Substances 0.000 abstract 1
Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01N—INVESTIGATING OR ANALYSING MATERIALS BY DETERMINING THEIR CHEMICAL OR PHYSICAL PROPERTIES
- G01N33/00—Investigating or analysing materials by specific methods not covered by groups G01N1/00 - G01N31/00
- G01N33/18—Water
- G01N33/1826—Organic contamination in water
- G01N33/1846—Total carbon analysis
-
- Y—GENERAL TAGGING OF NEW TECHNOLOGICAL DEVELOPMENTS; GENERAL TAGGING OF CROSS-SECTIONAL TECHNOLOGIES SPANNING OVER SEVERAL SECTIONS OF THE IPC; TECHNICAL SUBJECTS COVERED BY FORMER USPC CROSS-REFERENCE ART COLLECTIONS [XRACs] AND DIGESTS
- Y02—TECHNOLOGIES OR APPLICATIONS FOR MITIGATION OR ADAPTATION AGAINST CLIMATE CHANGE
- Y02A—TECHNOLOGIES FOR ADAPTATION TO CLIMATE CHANGE
- Y02A20/00—Water conservation; Efficient water supply; Efficient water use
- Y02A20/20—Controlling water pollution; Waste water treatment
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- Health & Medical Sciences (AREA)
- Life Sciences & Earth Sciences (AREA)
- Chemical & Material Sciences (AREA)
- Engineering & Computer Science (AREA)
- Food Science & Technology (AREA)
- Medicinal Chemistry (AREA)
- Physics & Mathematics (AREA)
- Analytical Chemistry (AREA)
- Biochemistry (AREA)
- General Health & Medical Sciences (AREA)
- General Physics & Mathematics (AREA)
- Immunology (AREA)
- Pathology (AREA)
- Physical Or Chemical Processes And Apparatus (AREA)
- Cultivation Of Seaweed (AREA)
Abstract
Disclosed is a methodology and a process for measuring oceanographic parameters that may be used to quantify carbon dioxide gas that is removed from the atmosphere by stimulating Phytoplankton growth in the open pelagic ocean through Ocean Iron Enrichment or other means. This process uses observations of chlorophyll to determine the photosynthetic activity of Phytoplankon in the pelagic ocean.
Phytoplankton growth is inhibited in many parts of the ocean due to a limitation in critical micro-nutrients such as Iron. By restoring these micro-nutrients into nutrient deficient regions, Phytoplankton growth may be stimulated. As Phytoplankton cells grow, they photosynthesize and thus convert light and carbon dioxide into chemical energy such as glucose and release oxygen. Through predation from other organisms, a component of these phytoplankton cells fall beneath the ocean deep thermocline and thus the carbon consumed by these cells may be considered sequestered from the atmosphere. This process and methodology uses observations of chlorophyll and established conversion metrics to estimate the total quantity of carbon dioxide that is sequestered from the atmosphere, and consequently may be used to determine a metric for carbon emission reduction credits.
Phytoplankton growth is inhibited in many parts of the ocean due to a limitation in critical micro-nutrients such as Iron. By restoring these micro-nutrients into nutrient deficient regions, Phytoplankton growth may be stimulated. As Phytoplankton cells grow, they photosynthesize and thus convert light and carbon dioxide into chemical energy such as glucose and release oxygen. Through predation from other organisms, a component of these phytoplankton cells fall beneath the ocean deep thermocline and thus the carbon consumed by these cells may be considered sequestered from the atmosphere. This process and methodology uses observations of chlorophyll and established conversion metrics to estimate the total quantity of carbon dioxide that is sequestered from the atmosphere, and consequently may be used to determine a metric for carbon emission reduction credits.
Description
Process and methodology for quantifying carbon offsets from Ocean Phytoplankton stimulation INVENTOR
Peter Gross, Oceanea Environmental Solutions Inc 207-1425 Marine Drive, West Vancouver, BC, V7T 1B9 Submitted provisionally in Canada on Wednesday, June 4, 2014 DESCRIPTION
This invention is a methodology and process that may be used by carbon offset credit organizations as an approved methodology or process to manifest the issuance of carbon offset credits.
Of said invention, this methodology and process uses measurements of chlorophyll of the sea surface, and beneath the sea surface to define the project boundary, and the quantity of chlorophyll within the project boundary.
The quantity of chlorophyll within the project boundary is used, through a conversion formula, to obtain the total carbon sequestration manifested by the project.
Peter Gross, Oceanea Environmental Solutions Inc 207-1425 Marine Drive, West Vancouver, BC, V7T 1B9 Submitted provisionally in Canada on Wednesday, June 4, 2014 DESCRIPTION
This invention is a methodology and process that may be used by carbon offset credit organizations as an approved methodology or process to manifest the issuance of carbon offset credits.
Of said invention, this methodology and process uses measurements of chlorophyll of the sea surface, and beneath the sea surface to define the project boundary, and the quantity of chlorophyll within the project boundary.
The quantity of chlorophyll within the project boundary is used, through a conversion formula, to obtain the total carbon sequestration manifested by the project.
Claims
Process and methodology for quantifying carbon offsets from Ocean Phytoplankton stimulation INVENTOR
Peter Gross, Oceanea Environmental Solutions Inc 207-1425 Marine Drive, West Vancouver, BC, V7T 1B9 Submitted provisionally in Canada on Wednesday, June 4, 2014Claim 1:
The Project boundary of this methodology and process is defined as a baroclinic mesoscale Ocean eddy located within a High Nutrient Low Chlorophyll (HNLC) pelagic Ocean area.
Claim 2:
Of Claim 1, a bio-available form of Iron compound will been placed into the Ocean eddy.
Claim 3:
Of Claim 1, the baroclinic mesoscale Ocean eddy shall be defined in size, shape, area and location, with Satellite Altimetry data also known as SSH (Sea Surface Height).
Claim 4:
Of claim 1, 2 & 3, the photosynthetic activity within the project boundary shall be measured using observations of Chlorophyll (Chl).
Claim 5:
Of Claim 4, Chl measurements shall be taken of the sea surface, and beneath the sea surface to a depth of not less than 100 meters.
Claim 6:
Of Claim 5, Chl measurements of the sea surface shall be taken using satellite observations of Chlorophyll A.
Claim 7:
Of claim 6, an alternative observation of sea surface Chl may be accomplished using manned or unmanned aircraft equipped for observations of Chlorophyll A.
Claim 8:
Of Claim 5, Chl measurements beneath the sea surface shall be accomplished using Autonomous Underwater Vehicles (AUV).
Claim 9:
Of Claim 8, an alternative observation of beneath the sea surface Chl may be accomplished using autonomous vertical profiling buoys or floats.
Claim 10:
Of Claim 2, a Baseline Chl concentration metric shall be defined as the average Chl concentration within the project boundary prior to the addition of bio-available Iron. This figure shall be represented by ChI B
Claim 11:
Of Claim 10 and Claim 2, a project volume shall be defined as the three dimensional volume that has originated from within the project boundary due to the addition of bio-available Iron Compound.
Claim 12:
Of claim 11, the addition of bio-available Iron Compound into the project volume shall generate an increase in Chl concentration above the baseline Chl defined by Chl B
Claim 13:
Of claim 12, the project volume shall be defined as the volume contained within a three dimensional volume defined by the sea surface, and extending downwards. Within this three dimensional volume, the project volume shall be defined as the volume wherein the Chl concentration has been elevated above ChI B concentration due to the addition of bio-available iron. The project volume shall be represented by Vp. See Fig Claim 14:
Of claim 13, the project volume V p boundary shall be defined by an elevation in Chl concentration above baseline ChI B defined by the Chlorophyll cutoff threshold Chl Th.
Claim 15:
A value of Chill, may be defined as:
Chl Th = [ChI B x 1.25]
Claim 16:
Of claim 15, the multiplier shown as 1.25 may be larger or smaller, as long as it allows a clear definition of the boundary between ChI B and Iron Compound induced Chl for defining the value of Chl Th.
Claim 17:
The total daily carbon sequestration of the project volume V p shall be the total Chlorophyll concentration within the project volume minus the baseline Chl concentration ChI B multiplied by a conversion factor 1& 2 such as a particulate organic carbon (POC) to chlorophyll ratio given as:
(POC/CHL = 32 mg mg-1 ].
For example Carbon sequestration daily shall be represented by C Dy Total Daily Chlorophyll concentration within the project volume shall be represented by ChI TD
C Dy = (ChI TD- ChI B) x [POC/CHL = 32 mg mg-1 ]
Claim 18:
Of claim 17, improved POC/CHL conversion ratios may be used as they are developed.
Claim 19:
Of claim 2, 17 and claim 18, the total project duration shall be defined as the number of days during which the Chlorophyll concentration within the project volume is measurably elevated above surrounding water outside of the project volume. When the concentration of Chl within the project volume drops to the same or lower level than Chl outside of the project volume, the project shall be considered terminated. The total project duration shall therefore be defined as the number of days from the introduction of bio-available iron into the project area, until project termination. This shall be expressed as DUR P.
Claim 20:
Of claim 19, 18, 17, 16 and 15, the total project carbon sequestration shall be defined as the daily carbon sequestration C Dy, calculated and summed each day, for the total project duration DUR P.
Total Carbon Sequestration shall be represented by CTOT
Claim 21:
Of claim 20, the total Carbon Dioxide sequestration of the project shall be the total Carbon Sequestration of the project, multiplied by the mass ratio of Carbon to carbon Dioxide.
Therefore, the Total Carbon Dioxide Sequestration shall be represented by Co2TOT
Co2TOT = C TOT x (44/12)
Peter Gross, Oceanea Environmental Solutions Inc 207-1425 Marine Drive, West Vancouver, BC, V7T 1B9 Submitted provisionally in Canada on Wednesday, June 4, 2014Claim 1:
The Project boundary of this methodology and process is defined as a baroclinic mesoscale Ocean eddy located within a High Nutrient Low Chlorophyll (HNLC) pelagic Ocean area.
Claim 2:
Of Claim 1, a bio-available form of Iron compound will been placed into the Ocean eddy.
Claim 3:
Of Claim 1, the baroclinic mesoscale Ocean eddy shall be defined in size, shape, area and location, with Satellite Altimetry data also known as SSH (Sea Surface Height).
Claim 4:
Of claim 1, 2 & 3, the photosynthetic activity within the project boundary shall be measured using observations of Chlorophyll (Chl).
Claim 5:
Of Claim 4, Chl measurements shall be taken of the sea surface, and beneath the sea surface to a depth of not less than 100 meters.
Claim 6:
Of Claim 5, Chl measurements of the sea surface shall be taken using satellite observations of Chlorophyll A.
Claim 7:
Of claim 6, an alternative observation of sea surface Chl may be accomplished using manned or unmanned aircraft equipped for observations of Chlorophyll A.
Claim 8:
Of Claim 5, Chl measurements beneath the sea surface shall be accomplished using Autonomous Underwater Vehicles (AUV).
Claim 9:
Of Claim 8, an alternative observation of beneath the sea surface Chl may be accomplished using autonomous vertical profiling buoys or floats.
Claim 10:
Of Claim 2, a Baseline Chl concentration metric shall be defined as the average Chl concentration within the project boundary prior to the addition of bio-available Iron. This figure shall be represented by ChI B
Claim 11:
Of Claim 10 and Claim 2, a project volume shall be defined as the three dimensional volume that has originated from within the project boundary due to the addition of bio-available Iron Compound.
Claim 12:
Of claim 11, the addition of bio-available Iron Compound into the project volume shall generate an increase in Chl concentration above the baseline Chl defined by Chl B
Claim 13:
Of claim 12, the project volume shall be defined as the volume contained within a three dimensional volume defined by the sea surface, and extending downwards. Within this three dimensional volume, the project volume shall be defined as the volume wherein the Chl concentration has been elevated above ChI B concentration due to the addition of bio-available iron. The project volume shall be represented by Vp. See Fig Claim 14:
Of claim 13, the project volume V p boundary shall be defined by an elevation in Chl concentration above baseline ChI B defined by the Chlorophyll cutoff threshold Chl Th.
Claim 15:
A value of Chill, may be defined as:
Chl Th = [ChI B x 1.25]
Claim 16:
Of claim 15, the multiplier shown as 1.25 may be larger or smaller, as long as it allows a clear definition of the boundary between ChI B and Iron Compound induced Chl for defining the value of Chl Th.
Claim 17:
The total daily carbon sequestration of the project volume V p shall be the total Chlorophyll concentration within the project volume minus the baseline Chl concentration ChI B multiplied by a conversion factor 1& 2 such as a particulate organic carbon (POC) to chlorophyll ratio given as:
(POC/CHL = 32 mg mg-1 ].
For example Carbon sequestration daily shall be represented by C Dy Total Daily Chlorophyll concentration within the project volume shall be represented by ChI TD
C Dy = (ChI TD- ChI B) x [POC/CHL = 32 mg mg-1 ]
Claim 18:
Of claim 17, improved POC/CHL conversion ratios may be used as they are developed.
Claim 19:
Of claim 2, 17 and claim 18, the total project duration shall be defined as the number of days during which the Chlorophyll concentration within the project volume is measurably elevated above surrounding water outside of the project volume. When the concentration of Chl within the project volume drops to the same or lower level than Chl outside of the project volume, the project shall be considered terminated. The total project duration shall therefore be defined as the number of days from the introduction of bio-available iron into the project area, until project termination. This shall be expressed as DUR P.
Claim 20:
Of claim 19, 18, 17, 16 and 15, the total project carbon sequestration shall be defined as the daily carbon sequestration C Dy, calculated and summed each day, for the total project duration DUR P.
Total Carbon Sequestration shall be represented by CTOT
Claim 21:
Of claim 20, the total Carbon Dioxide sequestration of the project shall be the total Carbon Sequestration of the project, multiplied by the mass ratio of Carbon to carbon Dioxide.
Therefore, the Total Carbon Dioxide Sequestration shall be represented by Co2TOT
Co2TOT = C TOT x (44/12)
Priority Applications (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| CA2853638A CA2853638A1 (en) | 2014-06-04 | 2014-06-04 | Process and methodology for quantifying carbon offsets from ocean phytoplankton stimulation |
Applications Claiming Priority (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| CA2853638A CA2853638A1 (en) | 2014-06-04 | 2014-06-04 | Process and methodology for quantifying carbon offsets from ocean phytoplankton stimulation |
Publications (1)
| Publication Number | Publication Date |
|---|---|
| CA2853638A1 true CA2853638A1 (en) | 2015-12-04 |
Family
ID=55086892
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| CA2853638A Abandoned CA2853638A1 (en) | 2014-06-04 | 2014-06-04 | Process and methodology for quantifying carbon offsets from ocean phytoplankton stimulation |
Country Status (1)
| Country | Link |
|---|---|
| CA (1) | CA2853638A1 (en) |
Cited By (4)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| WO2016090479A1 (en) * | 2014-12-09 | 2016-06-16 | Oceaneos Environmental Solutions, Inc. | Non radioactive iron isotopes and method for use in tracing marine species |
| CN109815962A (en) * | 2019-01-17 | 2019-05-28 | 南京信息工程大学 | A method to identify chlorophyll ring structures at the edges of ocean eddies |
| CN113126633A (en) * | 2019-12-30 | 2021-07-16 | 中国科学院沈阳自动化研究所 | Zero-attack-angle depth-keeping navigation control method for light long-range AUV (autonomous Underwater vehicle) |
| US11774255B2 (en) | 2019-03-07 | 2023-10-03 | Greenlines Technology Inc. | Methods and systems for conversion of physical movements to carbon units |
-
2014
- 2014-06-04 CA CA2853638A patent/CA2853638A1/en not_active Abandoned
Cited By (6)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| WO2016090479A1 (en) * | 2014-12-09 | 2016-06-16 | Oceaneos Environmental Solutions, Inc. | Non radioactive iron isotopes and method for use in tracing marine species |
| CN109815962A (en) * | 2019-01-17 | 2019-05-28 | 南京信息工程大学 | A method to identify chlorophyll ring structures at the edges of ocean eddies |
| CN109815962B (en) * | 2019-01-17 | 2022-12-23 | 南京信息工程大学 | A method for identifying chlorophyll ring structures at the edge of an ocean eddy |
| US11774255B2 (en) | 2019-03-07 | 2023-10-03 | Greenlines Technology Inc. | Methods and systems for conversion of physical movements to carbon units |
| CN113126633A (en) * | 2019-12-30 | 2021-07-16 | 中国科学院沈阳自动化研究所 | Zero-attack-angle depth-keeping navigation control method for light long-range AUV (autonomous Underwater vehicle) |
| CN113126633B (en) * | 2019-12-30 | 2022-05-06 | 中国科学院沈阳自动化研究所 | A zero-angle-of-attack fixed-depth navigation control method for a light long-range AUV |
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Legal Events
| Date | Code | Title | Description |
|---|---|---|---|
| FZDE | Dead |
Effective date: 20160606 |