cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.1185520
title: Syntheses and coordination isomerism of heteroleptic divalent-metal (M = Co, Zn) carbazate complexes

description: Three heteroleptic divalent-metal alkyl-carbazate-thiocyanate complexes, [M(NCS)<sub>2</sub>(NH<sub>2</sub>NHCOOR)<sub>2</sub>] [M = Co and R = CH<sub>2</sub>CH<sub>3</sub> (<b>1</b>); M = Co and R = CH<sub>3</sub> (<b>2</b>); M = Zn and R = CH<sub>3</sub> (<b>3</b>)], have been prepared and characterized, and their crystal structures determined. In <b>1</b>, Co(II) adopts a fairly regular centrosymmetric <i>trans</i>-CoO<sub>2</sub>N<sub>4</sub> octahedral geometry arising from its coordination by two N,O-bidentate ethylcarbazate ligands and two <i>trans</i> N-bonded thiocyanates. In isostructural <b>2</b> and <b>3</b>, the metals adopt distorted <i>cis</i>-MO<sub>2</sub>N<sub>4</sub> octahedral geometries arising from two N,O-bidentate methylcarbazate ligands with <i>cis</i> N-bonded thiocyanates. The crystal structures feature N–H⋯O and N–H⋯S interactions. Thermal analysis data show that these compounds begin to decompose at temperatures between 130 and 160 °C. Crystal data: <b>1</b>, CoC<sub>8</sub>H<sub>16</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 383.32, <i>P2</i><sub><i>1</i></sub><i>/n</i> (No. 14), <i>a</i> = 5.2599(3) Å, <i>b</i> = 7.4209(4) Å, <i>c</i> = 20.1948(12) Å, <i>β</i> = 94.070(1)°, <i>V</i> = 786.28(8) Å<sup>3</sup>, <i>Z</i> = 2, <i>R</i>(<i>F</i>) = 0.028, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.073; <b>2</b>, CoC<sub>6</sub>H<sub>12</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 355.27, <i>P2</i><sub><i>1</i></sub><i>/n</i> (No. 14), <i>a</i> = 7.8663(3) Å, <i>b</i> = 10.5804(3) Å, <i>c</i> = 17.6313(5) Å, <i>β</i> = 102.019(10)°, <i>V</i> = 1435.26(8) Å<sup>3</sup>, <i>Z</i> = 4, <i>R</i>(<i>F</i>) = 0.036, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.097; <b>3</b>, ZnC<sub>6</sub>H<sub>12</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 361.71, <i>P2</i><sub><i>1</i></sub><i>/n</i> (No. 14), <i>a</i> = 7.8883(2) Å, <i>b</i> = 10.5756(3) Å, <i>c</i> = 17.5827(5) Å, <i>β</i> = 101.676(1)°, <i>V</i> = 1436.46(7) Å<sup>3</sup>, <i>Z</i> = 4, <i>R</i>(<i>F</i>) = 0.031, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.084.
DOI: 10.6084/m9.figshare.1185535.v1
title: Increase in rare earth element concentrations controlled by dissolved organic matter in river water during rainfall events in a temperate, small forested catchment

description: The distributions of dissolved rare earth elements (REEs) in river water during rainfall events in a forested catchment were studied to contribute to understandings of TRUs behavior. Variations in the concentrations of dissolved REEs and several elements (As, Sb, and V) apparently correlated well with peak intensities in the optical spectra (ultraviolet absorption and fluorescence emission) of the river water. The optical properties were considered to represent humic substances in dissolved organic matter (DOM). Similar hysteretic loops were found for the REE concentrations and optical intensities as a function of the water discharge. This result indicates that the mobile REEs and DOM likely shared flow paths from the soil to the stream during these events. An ultrafiltration study revealed that colloidal REEs present in a size fraction of 10–30 kilodaltons comprised the major component of the dissolved REEs and increased under high water flow. Considering these observations and model interpretations in the precedent literature, complexation of the dissolved REEs with DOM was suggested to occur during the studied rainfall events. A high correlation between the size-fractionated REE concentrations and specific ultraviolet absorbance was observed, suggesting that the aromaticity of DOM plays a role in its complexation with dissolved REEs.
DOI: 10.6084/m9.figshare.1185518
title: Dataset 3 gathered in York university woodlots

description: On September 22nd, 2014 around 3:00 pm with sunny weather, we as a group of four (Farnaz, Bahar, Tiffani, and Danny) headed to the York university's woodlots at Keele campus. We collected data for four datasets whereas dataset three is presented here. Starting at the edge of the woodlot, 10 pairs of trees were measured in circumference at breast height and the distance each pair were apart from each other. The first tree in each pair (referred to the main tree hereafter) is chosen as it is encountered walking a straight line from the edge of the woodlot to the centre. The second tree in pair refers to the closest tree to the main tree, in any direction. The main tree's circumference was measured first, using a transect measuring tape; followed by measuring the distance between the main and the closest tree to it. Then the circumference of the second tree was measured and recorded. The condition of each tree was also determined using its healthiness and canopy from 0-2, 2 being a tree with a huge green canopy (less than 40% sky seen). The same process was replicated for another 9 pairs of trees and the data collected were recorded and later transferred to an excel file where the diameter at breast height for all 20 trees was calculated to four decimal places; using the formula diameter=circumference/3.1416.
DOI: 10.6084/m9.figshare.1185518.v1
title: Dataset 3 gathered in York university woodlots

description: On September 22nd, 2014 around 3:00 pm with sunny weather, we as a group of four (Farnaz, Bahar, Tiffani, and Danny) headed to the York university's woodlots at Keele campus. We collected data for four datasets whereas dataset three is presented here. Starting at the edge of the woodlot, 10 pairs of trees were measured in circumference at breast height and the distance each pair were apart from each other. The first tree in each pair (referred to the main tree hereafter) is chosen as it is encountered walking a straight line from the edge of the woodlot to the centre. The second tree in pair refers to the closest tree to the main tree, in any direction. The main tree's circumference was measured first, using a transect measuring tape; followed by measuring the distance between the main and the closest tree to it. Then the circumference of the second tree was measured and recorded. The condition of each tree was also determined using its healthiness and canopy from 0-2, 2 being a tree with a huge green canopy (less than 40% sky seen). The same process was replicated for another 9 pairs of trees and the data collected were recorded and later transferred to an excel file where the diameter at breast height for all 20 trees was calculated to four decimal places; using the formula diameter=circumference/3.1416.
DOI: 10.6084/m9.figshare.1185535.v3
title: Increase in rare earth element concentrations controlled by dissolved organic matter in river water during rainfall events in a temperate, small forested catchment

description: The distributions of dissolved rare earth elements (REEs) in river water during rainfall events in a forested catchment were studied to contribute to understandings of TRUs behavior. Variations in the concentrations of dissolved REEs and several elements (As, Sb, and V) apparently correlated well with peak intensities in the optical spectra (ultraviolet absorption and fluorescence emission) of the river water. The optical properties were considered to represent humic substances in dissolved organic matter (DOM). Similar hysteretic loops were found for the REE concentrations and optical intensities as a function of the water discharge. This result indicates that the mobile REEs and DOM likely shared flow paths from the soil to the stream during these events. An ultrafiltration study revealed that colloidal REEs present in a size fraction of 10–30 kilodaltons comprised the major component of the dissolved REEs and increased under high water flow. Considering these observations and model interpretations in the precedent literature, complexation of the dissolved REEs with DOM was suggested to occur during the studied rainfall events. A high correlation between the size-fractionated REE concentrations and specific ultraviolet absorbance was observed, suggesting that the aromaticity of DOM plays a role in its complexation with dissolved REEs.
DOI: 10.6084/m9.figshare.1185516
title: Lab 2 - dataset 4

description: In this experiment, 10 randomly selected adult trees of the same species (yellow birch) were selected in the woodlot to gather data. The diameter at the breast height was measured in centimeters for both the adult trees and their respective nearest saplings through transect measuring tape. Moreover, the distance between the adult trees and their nearest sapling trees was also measured in centimeters through transect measuring tape. I hypothesize that the average distance between the adult tree and its sapling is lower as compared to the sapling of different specie because the seeds from the same specie fall and germinate in the close proximity of the adult tree. The canopy coverage of the adult trees was estimated by forming a quadrant through fingers and pointing it towards the branches or leaves to see how much sky can be seen. Based on the coverage, a percent value was recorded. This experiment was done in groups of 3-4. Our group members included Sana Jamal, Ferinaz, Afraa Tarafdar and Maham Anees (me). Furthermore I and Sana gathered the data in woodlot, whereas Farinaz and Afraa collected the data in grassland. The data was collected on Friday September 26, 2014 on Keele campus of York University between 2:30 pm to 5:00 pm. The temperature was about 20ᵒC and it was mainly sunny.
DOI: 10.6084/m9.figshare.1185521.v1
title: New Approaches in Joint

description: New Approaches
DOI: 10.6084/m9.figshare.1185520.v1
title: Syntheses and coordination isomerism of heteroleptic divalent-metal (M = Co, Zn) carbazate complexes

description: Three heteroleptic divalent-metal alkyl-carbazate-thiocyanate complexes, [M(NCS)<sub>2</sub>(NH<sub>2</sub>NHCOOR)<sub>2</sub>] [M = Co and R = CH<sub>2</sub>CH<sub>3</sub>; (<b>1</b>) M = Co and R = CH<sub>3</sub> (<b>2</b>); M = Zn and R = CH<sub>3</sub> (<b>3</b>)], have been prepared and characterized, and their crystal structures determined. In <b>1</b>, Co(II) adopts a fairly regular centrosymmetric <i>trans</i>-CoO<sub>2</sub>N<sub>4</sub> octahedral geometry arising from its coordination by two N,O-bidentate ethylcarbazate ligands and two <i>trans</i> N-bonded thiocyanates. In isostructural <b>2</b> and <b>3</b>, the metals adopt distorted <i>cis</i>-MO<sub>2</sub>N<sub>4</sub> octahedral geometries arising from two N,O-bidentate methylcarbazate ligands with <i>cis</i> N-bonded thiocyanates. The crystal structures feature N–H O and N–H S interactions. Thermal analysis data show that these compounds begin to decompose at temperatures between 130 °C and 160°C. Crystal data: <b>1</b>, CoC<sub>8</sub>H<sub>16</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 383.32, <i>P</i>2<sub>1</sub>/<i>n</i> (No. 14), <i>a</i> = 5.2599(3) Å, <i>b</i> = 7.4209(4) Å, <i>c</i> = 20.1948(12) Å, β = 94.070(1)°, <i>V</i> = 786.28(8) Å<sup>3</sup>, <i>Z</i> = 2, <i>R</i>(<i>F</i>) = 0.028, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.073; <b>2</b>, CoC<sub>6</sub>H<sub>12</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 355.27, <i>P</i>2<sub>1</sub>/<i>n</i> (No. 14), <i>a</i> = 7.8663(3) Å, <i>b</i> = 10.5804(3) Å, <i>c</i> = 17.6313(5) Å, β = 102.019(10)°, <i>V</i> = 1435.26(8) Å<sup>3</sup>, <i>Z</i> = 4, <i>R</i>(<i>F</i>) = 0.036, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.097; <b>3</b>, ZnC<sub>6</sub>H<sub>12</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 361.71, <i>P</i>2<sub>1</sub>/<i>n</i> (No. 14), a = 7.8883(2) Å, <i>b</i> = 10.5756(3) Å, <i>c</i> = 17.5827(5) Å, β = 101.676(1)°, <i>V</i> = 1436.46(7) Å<sup>3</sup>, <i>Z</i> = 4, <i>R</i>(<i>F</i>) = 0.031, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.084.
DOI: 10.6084/m9.figshare.1185535.v2
title: Increase in rare earth element concentrations controlled by dissolved organic matter in river water during rainfall events in a temperate, small forested catchment

description: The distributions of dissolved rare earth elements (REEs) in river water during rainfall events in a forested catchment were studied to contribute to understandings of TRUs behavior. Variations in the concentrations of dissolved REEs and several elements (As, Sb, and V) apparently correlated well with peak intensities in the optical spectra (ultraviolet absorption and fluorescence emission) of the river water. The optical properties were considered to represent humic substances in dissolved organic matter (DOM). Similar hysteretic loops were found for the REE concentrations and optical intensities as a function of the water discharge. This result indicates that the mobile REEs and DOM likely shared flow paths from the soil to the stream during these events. An ultrafiltration study revealed that colloidal REEs present in a size fraction of 10–30 kilodaltons comprised the major component of the dissolved REEs and increased under high water flow. Considering these observations and model interpretations in the precedent literature, complexation of the dissolved REEs with DOM was suggested to occur during the studied rainfall events. A high correlation between the size-fractionated REE concentrations and specific ultraviolet absorbance was observed, suggesting that the aromaticity of DOM plays a role in its complexation with dissolved REEs.
DOI: 10.6084/m9.figshare.1185521.v3
title: New Approaches in Joint

description: New Approaches
DOI: 10.6084/m9.figshare.1185514
title: WoodLot Data Set 4

description: data set number 4
DOI: 10.6084/m9.figshare.1185516.v2
title: Lab 2 - dataset 4

description: In this experiment, 10 randomly selected adult trees of the same species (yellow birch) were selected in the woodlot to gather data. The diameter at the breast height was measured in centimeters for both the adult trees and their respective nearest saplings through transect measuring tape. Moreover, the distance between the adult trees and their nearest sapling trees was also measured in centimeters through transect measuring tape. I hypothesize that the average distance between the adult tree and its sapling is lower as compared to the sapling of different specie because the seeds from the same specie fall and germinate in the close proximity of the adult tree. The canopy coverage of the adult trees was estimated by forming a quadrant through fingers and pointing it towards the branches or leaves to see how much sky can be seen. Based on the coverage, a percent value was recorded. This experiment was done in groups of 3-4. Our group members included Sana Jamal, Ferinaz, Afraa Tarafdar and Maham Anees (me). Furthermore I and Sana gathered the data in woodlot, whereas Farinaz and Afraa collected the data in grassland. The data was collected on Friday September 26, 2014 on Keele campus of York University between 2:30 pm to 5:00 pm. The temperature was about 20ᵒC and it was mainly sunny.
DOI: 10.6084/m9.figshare.1185520.v3
title: Syntheses and coordination isomerism of heteroleptic divalent-metal (M = Co, Zn) carbazate complexes

description: Three heteroleptic divalent-metal alkyl-carbazate-thiocyanate complexes, [M(NCS)<sub>2</sub>(NH<sub>2</sub>NHCOOR)<sub>2</sub>] [M = Co and R = CH<sub>2</sub>CH<sub>3</sub> (<b>1</b>); M = Co and R = CH<sub>3</sub> (<b>2</b>); M = Zn and R = CH<sub>3</sub> (<b>3</b>)], have been prepared and characterized, and their crystal structures determined. In <b>1</b>, Co(II) adopts a fairly regular centrosymmetric <i>trans</i>-CoO<sub>2</sub>N<sub>4</sub> octahedral geometry arising from its coordination by two N,O-bidentate ethylcarbazate ligands and two <i>trans</i> N-bonded thiocyanates. In isostructural <b>2</b> and <b>3</b>, the metals adopt distorted <i>cis</i>-MO<sub>2</sub>N<sub>4</sub> octahedral geometries arising from two N,O-bidentate methylcarbazate ligands with <i>cis</i> N-bonded thiocyanates. The crystal structures feature N–H⋯O and N–H⋯S interactions. Thermal analysis data show that these compounds begin to decompose at temperatures between 130 and 160 °C. Crystal data: <b>1</b>, CoC<sub>8</sub>H<sub>16</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 383.32, <i>P2</i><sub><i>1</i></sub><i>/n</i> (No. 14), <i>a</i> = 5.2599(3) Å, <i>b</i> = 7.4209(4) Å, <i>c</i> = 20.1948(12) Å, <i>β</i> = 94.070(1)°, <i>V</i> = 786.28(8) Å<sup>3</sup>, <i>Z</i> = 2, <i>R</i>(<i>F</i>) = 0.028, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.073; <b>2</b>, CoC<sub>6</sub>H<sub>12</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 355.27, <i>P2</i><sub><i>1</i></sub><i>/n</i> (No. 14), <i>a</i> = 7.8663(3) Å, <i>b</i> = 10.5804(3) Å, <i>c</i> = 17.6313(5) Å, <i>β</i> = 102.019(10)°, <i>V</i> = 1435.26(8) Å<sup>3</sup>, <i>Z</i> = 4, <i>R</i>(<i>F</i>) = 0.036, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.097; <b>3</b>, ZnC<sub>6</sub>H<sub>12</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 361.71, <i>P2</i><sub><i>1</i></sub><i>/n</i> (No. 14), <i>a</i> = 7.8883(2) Å, <i>b</i> = 10.5756(3) Å, <i>c</i> = 17.5827(5) Å, <i>β</i> = 101.676(1)°, <i>V</i> = 1436.46(7) Å<sup>3</sup>, <i>Z</i> = 4, <i>R</i>(<i>F</i>) = 0.031, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.084.
DOI: 10.6084/m9.figshare.1185521.v2
title: New Approaches in Joint

description: New Approaches
DOI: 10.6084/m9.figshare.1185513
title: Techniques & data: field training with plants. Woodlot dataset 4

description: Recordings of Acer negundo canopy coverage, diameter at breast height(dbh), the distance to the nearest sapling and its dbh were conducted at Saywell Woods located at York University on Monday September 22 2014 at approximately 4:15pm. The temperature was 14 degrees Celcius with sunshine and wind.
DOI: 10.6084/m9.figshare.1185513.v1
title: Techniques & data: field training with plants. Woodlot dataset 4

description: Recordings of Acer negundo canopy coverage, diameter at breast height(dbh), the distance to the nearest sapling and its dbh were conducted at Saywell Woods located at York University on Monday September 22 2014 at approximately 4:15pm. The temperature was 14 degrees Celcius with sunshine and wind.
DOI: 10.6084/m9.figshare.1185514.v1
title: WoodLot Data Set 4

description: data set number 4
DOI: 10.6084/m9.figshare.1185516.v1
title: Lab 2 - dataset 4

description: In this experiment, 10 randomly selected adult trees of the same species (yellow birch) were selected in the woodlot to gather data. The diameter at the breast height was measured in centimeters for both the adult trees and their respective nearest saplings through transect measuring tape. Moreover, the distance between the adult trees and their nearest sapling trees was also measured in centimeters through transect measuring tape. I hypothesize that the average distance between the adult tree and its sapling is lower as compared to the sapling of different specie because the seeds from the same specie fall and germinate in the close proximity of the adult tree. The canopy coverage of the adult trees was estimated by forming a quadrant through fingers and pointing it towards the branches or leaves to see how much sky can be seen. Based on the coverage, a percent value was recorded. This experiment was done in groups of 3-4. Our group members included Sana Jamal, Ferinaz, Afraa Tarafdar and Maham Anees (me). Furthermore I and Sana gathered the data in woodlot, whereas Farinaz and Afraa collected the data in grassland. The data was collected on Friday September 26, 2014 on Keele campus of York University between 2:30 pm to 5:00 pm. The temperature was about 20ᵒC and it was mainly sunny.
DOI: 10.6084/m9.figshare.1185520.v2
title: Syntheses and coordination isomerism of heteroleptic divalent-metal (M = Co, Zn) carbazate complexes

description: Three heteroleptic divalent-metal alkyl-carbazate-thiocyanate complexes, [M(NCS)<sub>2</sub>(NH<sub>2</sub>NHCOOR)<sub>2</sub>] [M = Co and R = CH<sub>2</sub>CH<sub>3</sub> (<b>1</b>); M = Co and R = CH<sub>3</sub> (<b>2</b>); M = Zn and R = CH<sub>3</sub> (<b>3</b>)], have been prepared and characterized, and their crystal structures determined. In <b>1</b>, Co(II) adopts a fairly regular centrosymmetric <i>trans</i>-CoO<sub>2</sub>N<sub>4</sub> octahedral geometry arising from its coordination by two N,O-bidentate ethylcarbazate ligands and two <i>trans</i> N-bonded thiocyanates. In isostructural <b>2</b> and <b>3</b>, the metals adopt distorted <i>cis</i>-MO<sub>2</sub>N<sub>4</sub> octahedral geometries arising from two N,O-bidentate methylcarbazate ligands with <i>cis</i> N-bonded thiocyanates. The crystal structures feature N–H⋯O and N–H⋯S interactions. Thermal analysis data show that these compounds begin to decompose at temperatures between 130 and 160 °C. Crystal data: <b>1</b>, CoC<sub>8</sub>H<sub>16</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 383.32, <i>P2</i><sub><i>1</i></sub><i>/n</i> (No. 14), <i>a</i> = 5.2599(3) Å, <i>b</i> = 7.4209(4) Å, <i>c</i> = 20.1948(12) Å, <i>β</i> = 94.070(1)°, <i>V</i> = 786.28(8) Å<sup>3</sup>, <i>Z</i> = 2, <i>R</i>(<i>F</i>) = 0.028, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.073; <b>2</b>, CoC<sub>6</sub>H<sub>12</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 355.27, <i>P2</i><sub><i>1</i></sub><i>/n</i> (No. 14), <i>a</i> = 7.8663(3) Å, <i>b</i> = 10.5804(3) Å, <i>c</i> = 17.6313(5) Å, <i>β</i> = 102.019(10)°, <i>V</i> = 1435.26(8) Å<sup>3</sup>, <i>Z</i> = 4, <i>R</i>(<i>F</i>) = 0.036, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.097; <b>3</b>, ZnC<sub>6</sub>H<sub>12</sub>N<sub>6</sub>O<sub>4</sub>S<sub>2</sub>, <i>M</i><sub>r</sub> = 361.71, <i>P2</i><sub><i>1</i></sub><i>/n</i> (No. 14), <i>a</i> = 7.8883(2) Å, <i>b</i> = 10.5756(3) Å, <i>c</i> = 17.5827(5) Å, <i>β</i> = 101.676(1)°, <i>V</i> = 1436.46(7) Å<sup>3</sup>, <i>Z</i> = 4, <i>R</i>(<i>F</i>) = 0.031, <i>wR</i>(<i>F</i><sup>2</sup>) = 0.084.
DOI: 10.6084/m9.figshare.1185512
title: Dataset 2 Transects on Grassland: measuring the purple Aster

description: Jehan Yousif Time: 2:30PM - 5:30 Date: 22 September 2014 Weather: 16°C Location: York University
DOI: 10.6084/m9.figshare.1185508
title: Ecology 2050 Grassland Dataset 2

description: The experiment was conducted at York University on September 26th, 2014 in grasslands adjacent to Danby Woods. The purpose of this experiment was to become comfortable with plant sampling methods used in Ecology studies. Using a trasect tape (30m), the distance between thistle plants was recorded, to within 1m on either side of the tape. The height of the plant, number of leaves, number of flowers, and level of crowding were also recorded for a sample size of n = 50. When there were no other plants found along the transect tape, the tape was relocated to a different<br>area. This data was collected in collaboration with other researchers Elron, Simmy, and Laiba.
DOI: 10.6084/m9.figshare.1185501
title: Lab 2: Observing plan diversity and field training (Dataset 1)

description: This field data was collected at the grasslands situated in York University. This research was done by a group of undergraduate students under the supervison of a T.A. We were provided with a metal quadrat(1mx1m) which was used to observe the following variables: abundance of plants, types of plant species, number of individual species, total cover of vegetation, and total cover of grass.
DOI: 10.6084/m9.figshare.1185512.v1
title: Dataset 2 Transects on Grassland: measuring the purple Aster

description: Jehan Yousif Time: 2:30PM - 5:30 Date: 22 September 2014 Weather: 16°C Location: York University
DOI: 10.6084/m9.figshare.1185496
title: Grassland Dataset 1 - Lab 01 - Group 1

description: Akhilesh Kadian; Techniques & Data.