{
    "document_id": 11804,
    "page": 11,
    "width_pt": 612,
    "height_pt": 792,
    "rotation": 0,
    "pipeline_version": "paddleocr-vl-1.6+paul-48",
    "engine": "paddleocr_vl",
    "source_run_id": 11915,
    "item_count": 9,
    "counts_by_type": {
        "footer": 1,
        "heading": 3,
        "text": 5
    },
    "build_ms": 1,
    "items": [
        {
            "id": "p11.1",
            "order": 1,
            "type": "text",
            "bbox": {
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                "r": 542.4,
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            "text": "Lakewood sand is coarse grained soil with high permeability and deep-water table. The series is well drained and typically imposes little to no limitations on site development. The BerAr-Berryland sand can typically have poor drainage soil, as water table may be close to the surface. Boring samples were completed at this site and the soils data revealed there was no limitation imposed on the site's development from the soil evaluation."
        },
        {
            "id": "p11.2",
            "order": 2,
            "type": "text",
            "bbox": {
                "l": 69.84,
                "t": 587.76,
                "r": 541.2,
                "b": 552.72
            },
            "text": "Soil test pits were performed by PDS at various locations to assess soil conditions and depth to seasonal high-water table. The test pit locations and logs are illustrated on the Site Plans."
        },
        {
            "id": "p11.3",
            "order": 3,
            "type": "heading",
            "bbox": {
                "l": 70.08,
                "t": 526.08,
                "r": 163.44,
                "b": 512.16
            },
            "text": "2.3 Vegetation",
            "attrs": {
                "block_label": "paragraph_title"
            },
            "level": 3
        },
        {
            "id": "p11.4",
            "order": 4,
            "type": "text",
            "bbox": {
                "l": 68.4,
                "t": 505.2,
                "r": 541.92,
                "b": 386.4
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            "text": "The subject property is currently occupied with a 2-story masonry building. The existing site has crushed asphalt milling with fenced in enclosers. There is also partially wooded area in the rear section of the property. Vegetation identified on the site include tree species such as White oak (Quercus alba), Eastern black oak (Quercus velutina), Pitch pine (Pinus rigida) and Chestnut Oak (Quercus). Any specimen trees present as defined by the Jackson Township Tree Ordinance have been located and identified on the Site Plans."
        },
        {
            "id": "p11.5",
            "order": 5,
            "type": "heading",
            "bbox": {
                "l": 69.6,
                "t": 360.48,
                "r": 179.52,
                "b": 346.8
            },
            "text": "2.4 Surface Water",
            "attrs": {
                "block_label": "paragraph_title"
            },
            "level": 3
        },
        {
            "id": "p11.6",
            "order": 6,
            "type": "text",
            "bbox": {
                "l": 105.36,
                "t": 339.12,
                "r": 534.96,
                "b": 325.44
            },
            "text": "There are no surface waters nor riparian buffers located on or adjacent to the subject site."
        },
        {
            "id": "p11.7",
            "order": 7,
            "type": "heading",
            "bbox": {
                "l": 70.08,
                "t": 298.08,
                "r": 196.32,
                "b": 284.88
            },
            "text": "2.5 Subsurface Water",
            "attrs": {
                "block_label": "paragraph_title"
            },
            "level": 3
        },
        {
            "id": "p11.8",
            "order": 8,
            "type": "text",
            "bbox": {
                "l": 68.64,
                "t": 276.96,
                "r": 543.12,
                "b": 75.84
            },
            "text": "The upper part of the Kirkwood Formation and the Cohansey Sand are hydraulically well connected and together function as an aquifer system. Underlying the Kirkwood-Cohansey aquifer system is the composite confining unit, a complex series of geologic units that, depending on location, can include as many as nine distinct units. The part of the composite confining unit of interest in this area ranges in age from Palecene to early Miocene and is made up of the Vincentown Formation, Manasquan Formation, Shark River Formation, Piney Point Formation, and basal clay of the Kirkwood Formation. Two minor aquifers are present in this part of the composite confining unit. The Vincentown aquifer consists of the Vincentown Formation, which is comprised of moderately permeable Quartz sand. The Vincentown aquifer is used as a source of water only in and near the outcrop areas, in the northwestern part of the County. The other minor aquifer, Piney Point Formation, is also present in this part of the State."
        },
        {
            "id": "p11.9",
            "order": 9,
            "type": "footer",
            "bbox": {
                "l": 302.16,
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                "r": 309.84,
                "b": 35.28
            },
            "text": "7",
            "attrs": {
                "block_label": "number"
            }
        }
    ],
    "excluded_furniture": {
        "first": [],
        "last": []
    }
}