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Markdownthe whole file · cited lines 74–76 and 97–103 marked
# Intertidal survey of Kellow Sands and Thrimby Point

Report BEP/SR/2026/11 · Survey of 19 to 23 January 2026 · Issued February 2026


# Summary

The four fixed transects at Kellow Sands and Thrimby Point were resurveyed in January, in the third winter
since sediment recharge began. This report sets out the method, the profiles measured, and the change on
each transect since the surveys began.


Levels were taken at five-metre intervals along each transect with a total station from the survey marks on
the training wall and at the lifeboat house. Sediment samples were taken at the mid-shore station on each
transect for particle size, and are reported by the laboratory separately.


Conditions during the survey were settled, with no swell and a spring range near the mean. Nothing about
the week's weather is likely to have affected the levels measured.


**Background**
The Partnership has surveyed the intertidal at Kellow Sands since 2019, when the four transects were
established to provide a baseline for the sediment recharge then being planned. The first two winters were
surveyed before any material was placed. Placement began in the winter of 2023/24 and has been carried
out in each winter since, most recently between November 2025 and January 2026.


The purpose of the survey is a narrow one. It is meant to answer whether the intertidal profile at Kellow
Sands is gaining or losing sediment, and at what rate, on lines whose position is fixed. It is not a study of
where the placed material goes, which would need tracer work the Partnership has not commissioned, and
it cannot by itself attribute a change to the recharge rather than to the weather.


**Method**
Levels were taken with a total station from the two survey marks used since 2019, at five-metre intervals
along each transect and at every break of slope between them. Each line was run twice, out and back, and
the two sets agreed everywhere within the tolerance the method allows. Where they did not, which
happened once on transect three, the point was re-observed.


The horizontal position of each line is fixed by a mark set in concrete at the landward end and by a pin in the
training wall or the marsh edge at the seaward end. All eight marks were found and checked against the
2019 coordinates before work began. The pin at the seaward end of transect two has moved and was
re-established from the landward mark; the correction is recorded in the level book and is smaller than the
interval between observations.


Sediment samples were taken at the mid-shore station on each line, in the order in which the lines were
surveyed, and delivered to the laboratory the same afternoon. Particle size is reported separately and is not
discussed here.


<!-- PAGE BREAK -->

**The transects**
Transect one runs from the seawall opposite the boatyard to the low water mark, crossing the widest part of
the sand. It is the longest of the four lines and the only one on which the whole intertidal profile can be
surveyed within a single tide.


Transects two and three are the pair the recharge was expected to affect. Both cross the placement
footprint at its northern end, transect two some sixty metres from the discharge point and transect three
about a hundred and forty. Neither has been moved since it was established, and the marks at both ends of
both lines were found in good order.


The plan below shows the four lines as they were surveyed in January, together with the saltmarsh edge as
it stood at the 1998 survey. The 1998 edge is drawn because it is the last edge surveyed on the ground
rather than taken from photography, and because it is the line against which the advisers have asked that
marsh extent be reported.


<figure type="DIAGRAM">Figure 1. Survey transects at Kellow Sands and Thrimby Point. Sampling stations are shown as filled circles and the 1998 saltmarsh edge as a broken line. 

<description>The diagram depicts a survey site map divided into two main areas: 'Kellow Sands' on the left and 'Thrimby Point' on the right, oriented with a North arrow pointing up. Four vertical survey transects (T1, T2, T3, T4) are drawn spanning the area. Each transect features three filled black circles representing sampling stations distributed along its length. A dashed line running horizontally across the transects represents the '1998 saltmarsh edge'. The lower boundary of the diagram is marked by a solid blue line above a light blue shaded region, while the upper boundary is defined by a light beige region containing the location labels.</description></figure>

Transect four crosses the toe of the training wall and has always behaved differently from the other three. It
is retained because the wall itself is the reason for the difference, and because the Partnership was asked
in 2019 to keep a line there.


The stations shown on the plan are those at which sediment samples are taken, and not the points at which
levels were observed: the level observations are too close together to plot at this scale. A full set of profiles
is bound into the copy of this report held by the secretariat.


<!-- PAGE BREAK -->

# Change since the first survey

Change is reported as a mean annual rate over each winter, taken across the whole intertidal part of the
line. Accretion varied markedly between transects, and the pattern is the same in each of the three winters
measured.


<figure type="CHART">Mean sediment accretion by transect, winters 2023/24 to 2025/26



<description>A grouped bar chart displaying mean sediment accretion in mm/yr across four transects over three winter periods: 2023/24 (dark grey), 2024/25 (medium grey), and 2025/26 (light grey). Transect 1 shows low positive accretion, Transect 2 shows the highest positive accretion, Transect 3 shows moderate positive accretion, and Transect 4 shows negative accretion (erosion) across all three years.</description>

<table><thead><tr><th>Transect</th><th>2023/24 (mm/yr)</th><th>2024/25 (mm/yr)</th><th>2025/26 (mm/yr)</th></tr></thead><tbody><tr><td>Transect 1</td><td>~0.4</td><td>~0.7</td><td>~0.6</td></tr><tr><td>Transect 2</td><td>~2.8</td><td>~3.5</td><td>~3.9</td></tr><tr><td>Transect 3</td><td>~1.9</td><td>~2.4</td><td>~3.0</td></tr><tr><td>Transect 4</td><td>~-0.6</td><td>~-0.7</td><td>~-1.0</td></tr></tbody></table></figure>

The rates plotted are means over the intertidal part of each line, weighted by the length of profile each
observation represents. A mean of that kind conceals a good deal. On transect two most of the gain is in the
upper third of the profile, and on transect four the loss is almost all at the toe of the wall; the profiles show
this plainly and a mean does not.


The advisers' view, which the secretariat shares, is that three winters is too short a run to separate the
effect of placement from the variation the estuary shows anyway. The transects should be resurveyed next
January on the same lines and by the same method before anything is concluded from them.


<!-- PAGE BREAK -->

**The next survey**
The profiles themselves, the level books and the mark check sheets are held by the secretariat and are
available to Partnership members on request.


The next survey is due in January 2027. The secretariat proposes to keep the January window, and to ask
the laboratory for particle size on the same four stations so that the series stays comparable.

<!-- doc_id=parse-01m22n4vxge28dz3xhhps3absp -->

Returned Markdown: the full converted survey report

Copied from Output file (Markdown), lines 74–76, 97–103

Open the Markdown file ↗
Output file (JSON)
Raw API response: Markdown, metadata and document structure
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Show the whole file (42 KB)
JSON
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  "markdown": "# Intertidal survey of Kellow Sands and Thrimby Point\n\nReport BEP/SR/2026/11 \u00b7 Survey of 19 to 23 January 2026 \u00b7 Issued February 2026\n\n\n# Summary\n\nThe four fixed transects at Kellow Sands and Thrimby Point were resurveyed in January, in the third winter\nsince sediment recharge began. This report sets out the method, the profiles measured, and the change on\neach transect since the surveys began.\n\n\nLevels were taken at five-metre intervals along each transect with a total station from the survey marks on\nthe training wall and at the lifeboat house. Sediment samples were taken at the mid-shore station on each\ntransect for particle size, and are reported by the laboratory separately.\n\n\nConditions during the survey were settled, with no swell and a spring range near the mean. Nothing about\nthe week's weather is likely to have affected the levels measured.\n\n\n**Background**\nThe Partnership has surveyed the intertidal at Kellow Sands since 2019, when the four transects were\nestablished to provide a baseline for the sediment recharge then being planned. The first two winters were\nsurveyed before any material was placed. Placement began in the winter of 2023/24 and has been carried\nout in each winter since, most recently between November 2025 and January 2026.\n\n\nThe purpose of the survey is a narrow one. It is meant to answer whether the intertidal profile at Kellow\nSands is gaining or losing sediment, and at what rate, on lines whose position is fixed. It is not a study of\nwhere the placed material goes, which would need tracer work the Partnership has not commissioned, and\nit cannot by itself attribute a change to the recharge rather than to the weather.\n\n\n**Method**\nLevels were taken with a total station from the two survey marks used since 2019, at five-metre intervals\nalong each transect and at every break of slope between them. Each line was run twice, out and back, and\nthe two sets agreed everywhere within the tolerance the method allows. Where they did not, which\nhappened once on transect three, the point was re-observed.\n\n\nThe horizontal position of each line is fixed by a mark set in concrete at the landward end and by a pin in the\ntraining wall or the marsh edge at the seaward end. All eight marks were found and checked against the\n2019 coordinates before work began. The pin at the seaward end of transect two has moved and was\nre-established from the landward mark; the correction is recorded in the level book and is smaller than the\ninterval between observations.\n\n\nSediment samples were taken at the mid-shore station on each line, in the order in which the lines were\nsurveyed, and delivered to the laboratory the same afternoon. Particle size is reported separately and is not\ndiscussed here.\n\n\n<!-- PAGE BREAK -->\n\n**The transects**\nTransect one runs from the seawall opposite the boatyard to the low water mark, crossing the widest part of\nthe sand. It is the longest of the four lines and the only one on which the whole intertidal profile can be\nsurveyed within a single tide.\n\n\nTransects two and three are the pair the recharge was expected to affect. Both cross the placement\nfootprint at its northern end, transect two some sixty metres from the discharge point and transect three\nabout a hundred and forty. Neither has been moved since it was established, and the marks at both ends of\nboth lines were found in good order.\n\n\nThe plan below shows the four lines as they were surveyed in January, together with the saltmarsh edge as\nit stood at the 1998 survey. The 1998 edge is drawn because it is the last edge surveyed on the ground\nrather than taken from photography, and because it is the line against which the advisers have asked that\nmarsh extent be reported.\n\n\n<figure type=\"DIAGRAM\">Figure 1. Survey transects at Kellow Sands and Thrimby Point. Sampling stations are shown as filled circles and the 1998 saltmarsh edge as a broken line. \n\n<description>The diagram depicts a survey site map divided into two main areas: 'Kellow Sands' on the left and 'Thrimby Point' on the right, oriented with a North arrow pointing up. Four vertical survey transects (T1, T2, T3, T4) are drawn spanning the area. Each transect features three filled black circles representing sampling stations distributed along its length. A dashed line running horizontally across the transects represents the '1998 saltmarsh edge'. The lower boundary of the diagram is marked by a solid blue line above a light blue shaded region, while the upper boundary is defined by a light beige region containing the location labels.</description></figure>\n\nTransect four crosses the toe of the training wall and has always behaved differently from the other three. It\nis retained because the wall itself is the reason for the difference, and because the Partnership was asked\nin 2019 to keep a line there.\n\n\nThe stations shown on the plan are those at which sediment samples are taken, and not the points at which\nlevels were observed: the level observations are too close together to plot at this scale. A full set of profiles\nis bound into the copy of this report held by the secretariat.\n\n\n<!-- PAGE BREAK -->\n\n# Change since the first survey\n\nChange is reported as a mean annual rate over each winter, taken across the whole intertidal part of the\nline. Accretion varied markedly between transects, and the pattern is the same in each of the three winters\nmeasured.\n\n\n<figure type=\"CHART\">Mean sediment accretion by transect, winters 2023/24 to 2025/26\n\n\n\n<description>A grouped bar chart displaying mean sediment accretion in mm/yr across four transects over three winter periods: 2023/24 (dark grey), 2024/25 (medium grey), and 2025/26 (light grey). Transect 1 shows low positive accretion, Transect 2 shows the highest positive accretion, Transect 3 shows moderate positive accretion, and Transect 4 shows negative accretion (erosion) across all three years.</description>\n\n<table><thead><tr><th>Transect</th><th>2023/24 (mm/yr)</th><th>2024/25 (mm/yr)</th><th>2025/26 (mm/yr)</th></tr></thead><tbody><tr><td>Transect 1</td><td>~0.4</td><td>~0.7</td><td>~0.6</td></tr><tr><td>Transect 2</td><td>~2.8</td><td>~3.5</td><td>~3.9</td></tr><tr><td>Transect 3</td><td>~1.9</td><td>~2.4</td><td>~3.0</td></tr><tr><td>Transect 4</td><td>~-0.6</td><td>~-0.7</td><td>~-1.0</td></tr></tbody></table></figure>\n\nThe rates plotted are means over the intertidal part of each line, weighted by the length of profile each\nobservation represents. A mean of that kind conceals a good deal. On transect two most of the gain is in the\nupper third of the profile, and on transect four the loss is almost all at the toe of the wall; the profiles show\nthis plainly and a mean does not.\n\n\nThe advisers' view, which the secretariat shares, is that three winters is too short a run to separate the\neffect of placement from the variation the estuary shows anyway. The transects should be resurveyed next\nJanuary on the same lines and by the same method before anything is concluded from them.\n\n\n<!-- PAGE BREAK -->\n\n**The next survey**\nThe profiles themselves, the level books and the mark check sheets are held by the secretariat and are\navailable to Partnership members on request.\n\n\nThe next survey is due in January 2027. The secretariat proposes to keep the January window, and to ask\nthe laboratory for particle size on the same four stations so that the series stays comparable.\n\n<!-- doc_id=parse-01m22n4vxge28dz3xhhps3absp -->",
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      {
        "type": "page",
        "grounding": {
          "page": 4,
          "range": {
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            "end": 7392
          },
          "box": {
            "xmin": 0.0,
            "ymin": 0.0,
            "xmax": 1.0,
            "ymax": 1.0
          }
        },
        "status": "ok",
        "children": [
          {
            "type": "text",
            "id": "text-17",
            "grounding": {
              "page": 4,
              "range": {
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                "end": 7188
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              "box": {
                "xmin": 0.09319,
                "ymin": 0.05607,
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                "ymax": 0.12669
              }
            },
            "atomic_grounding": [
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                },
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                }
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            "id": "text-18",
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              },
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  }
}
Open the JSON file ↗
Expected vs. Found
✗Expected: The chart preserved as an image in position with its title; added textual data is optional.Found: The title remained in place, followed by a description and table, but the chart image was not returned.
Supporting proof
Proof 1Screenshot
Source and output comparison: the survey chart and its converted page
Open original ↗
Proof 2Screenshot
Run card: result, timing, conditions and input
Open original ↗
Why this result

The chart needed to remain an image with its title. The complete PDF was converted successfully, but the image was absent, so this is a fail rather than a missing result. The endpoint has no supported option for returning the chart image.

Also observed in this test case

Approximate chart values. The sediment accretion chart’s table contains twelve values corresponding to the plotted bars, each marked as approximate.

Tested by Chandresh Bisht · evidence dated 9 September 2026

Configuration and setup

How this tool was set up for the run and what the test needed in place. Each row is a fact from the run's records; a fact the records do not hold is left out, not guessed.

Software that produced the output
Landing AI
Build or version
ADE Parse API v2; model_version dpt-3-pro-20260710
Plan or tier
Explore (free tier)
Surface
API
Set up before the run
A PDF with a titled data chart was required. The complete PDF was to be converted to Markdown in one pass using the default pipeline, without per-tool flag tuning.
Pipeline
default pipeline; no model or options overrides · single pass
Tested
9 September 2026 · Chandresh Bisht

How this scenario is graded

How we decide Pass, Fail and Not gradable. The same rules apply to every tool tested on this scenario.

How results are decided

Each test case gets one result per tool: Pass, Fail or Not gradable. A test case we haven't run yet shows Untested. There are no partial results.

The rules
  • Pass: the tool did everything the test expected, and nothing it said contradicts the correct answer.
  • Fail: at least one expected behaviour clearly didn't happen; the test case's result says which one and quotes the tool.
  • Not gradable: our evidence couldn't settle the outcome (for example a record we needed is missing). It is never counted as a fail, and the test case's result says what's missing.

Where this sits in the benchmark

This page is one cell of a larger study: one tool, one scenario. Only this benchmark's frame appears here.

History of this result

What has happened to this result since it was first published. Runs and grades are never overwritten: a retest or a re-grade publishes a new result and keeps the earlier one readable.

from the publication record
11 November 2026First publishedConverting a complex PDF into clean Markdown with a hosted API v1

Act on this result

Nothing filed here edits the run or the grade. A challenge opens a review, and a review can produce a new run or a re-grade — which becomes the current result and leaves this one in the history.

This matches what I see

You run the same kind of test against your own setup and get the same behaviour.

Agree →
This does not match

Yours behaves differently. Tell us what you got, with a screenshot if you have one.

Disagree →
Point out an issue

Something here is wrong — a reference value, a transcription, a grade.

Report an issue →
Request a retest

On a newer build, a larger dataset, or your own setup.

Request a retest →
We have fixed this

Tell us what changed and we schedule a rerun of the failing test case. The old result stays as history.

Vendor notice →
Filed against this evidenceNothing yet. Challenges, counter-evidence and fix notices appear here with their outcome, and stay on the page after they are resolved.
Cite this result
aidemos.com/benchmarks/pdf-to-markdown-apis/results/landing-ai/a-document-with-a-data-chart · 0 pass · 1 fail · coverage 1/1 · graded 2026-10-30

The same record is available as structured data through the AI Demos MCP server, with the counts, the coverage and every per-test-case reason carried as fields.

Verify the proof files

These files support this result. Open a file to inspect the original evidence.

Input · Document (PDF) ↗application/pdf · 301 KB
Proof 1 · Screenshot ↗image/png · 304 KB
Output file (Markdown) ↗text/markdown · 7 KB
Output file (JSON) ↗application/json · 42 KB
Proof 2 · Screenshot ↗image/png · 96 KB
File fingerprints (SHA-256)

A fingerprint identifies the exact file used for this result.

Input · Document (PDF)75b2bcc613580942d7d3222254c0f0d084525c2c6521f55cffa629c49f64c608
Proof 1 · Screenshot9c23ae68ba6306ad4442e0de440fc2489ef871345a3ab30f6f30f6ee3038f1e3
Output file (Markdown)fa9a51a5ff27b127055252ef20657c0e9091f8eb0cf363e3492dc01c6fecd6c4
Output file (JSON)f463914cdea1a218b78bca9bbf6b2f4235291a9794f05f901096b806424ee56f
Proof 2 · Screenshot979c8983c79ed2ac94711367a65f0f50f426cbd64b207e6db96e631c48113755