cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.30031475
title: RThe_Plane_Plotter from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031475.v1
title: RThe_Plane_Plotter from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031478.v1
title: NS-FS-RThe-Plane from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031478
title: NS-FS-RThe-Plane from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031481
title: NS-NS-RZ-Plane from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031481.v1
title: NS-NS-RZ-Plane from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031484
title: FS-FS-RZ-Plane from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031484.v1
title: FS-FS-RZ-Plane from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031487
title: RZ_Plane_Plotter from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031487.v1
title: RZ_Plane_Plotter from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031490.v1
title: NS-FS-RZ-Plane from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.6084/m9.figshare.30031490
title: NS-FS-RZ-Plane from Elastic displacements and viscous hydrodynamic flows in wedge-shaped geometries with a straight edge: Green’s functions for parallel forces

description: For homogeneous and isotropic linearly elastic solids and for incompressible fluids under low-Reynolds-number conditions, the fundamental solutions of the associated continuum equations were derived a long time ago for bulk systems. That is, the corresponding Green’s functions are available in infinitely extended systems, where boundaries do not play any role. However, introducing boundaries renders the situation significantly more complex. Here, we derive the corresponding Green’s functions for a linearly elastic homogeneous and isotropic material in a wedge-shaped geometry. Two flat boundaries confine the material and meet at a straight edge. No-slip (NOS) and free-slip (FRS) conditions are considered. The force is oriented in a direction parallel to the straight edge of the wedge. Assuming incompressibility, our expressions also apply to the situation of low-Reynolds-number hydrodynamic viscous fluid flows. Thus, they may be used, for instance, to describe the motion of self-propelled objects guided by an edge or the distortion of soft elastic actuators in wedge-shaped environments of operation.
DOI: 10.15468/dl.rdp65t
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query:
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 "TaxonKey is one of (Tachysurus longispinalis)",
 "BasisOfRecord is one of (Specimen, Literature Occurrence, Human Observation, Observation)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "Year is greater than or equal to 1991",
 "Year is less than or equal to 2025"
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 The dataset includes 0 records from 0 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0019138-250827131500795/datasets/export for details.
DOI: 10.6084/m9.figshare.28613751
title: Changes in Intention to Quit Among Child Welfare and Protection Workers in Norway - How Does Time and Mentoring Affect Intention?

description: This longitudinal study examined the intention to quit (ITQ) among child welfare and protection (CWP) workers in Norway and its relationship with mentoring. Participants from 80 municipalities were surveyed at three time points (T1: <i>n</i> = 225, T2: <i>n</i> = 168, T3: <i>n</i> = 64). Linear mixed models revealed an increasing ITQ over time, with no significant impact of mentoring on ITQ trajectories or levels. Despite theoretical support for mentoring’s role in retention, variations in mentoring’s frequency, duration, and content may explain its lack of effect. The study suggests that future research should employ an experimental design to isolate the influence of specific mentoring attributes on CWP workers’ ITQ. Professional mentoring is proposed as a strategy to reduce turnover intentions.The term “mentoring” is frequently used interchangeably with guidance, coaching, and clinical or supportive supervision, varying by professional domain.The absence of a clear and universally accepted definition of mentoring leads to diverse practices and variations in both the content delivered and the qualifications of mentors.As currently implemented in Norwegian Child Welfare Services, mentoring is insufficient in addressing the increasing tendency of CWP workers to consider leaving their positions over time. Professional mentoring is proposed as a strategy to reduce turnover intentions. The term “mentoring” is frequently used interchangeably with guidance, coaching, and clinical or supportive supervision, varying by professional domain. The absence of a clear and universally accepted definition of mentoring leads to diverse practices and variations in both the content delivered and the qualifications of mentors. As currently implemented in Norwegian Child Welfare Services, mentoring is insufficient in addressing the increasing tendency of CWP workers to consider leaving their positions over time.
DOI: 10.6084/m9.figshare.28613751.v1
title: Changes in Intention to Quit Among Child Welfare and Protection Workers in Norway - How Does Time and Mentoring Affect Intention?

description: This longitudinal study examined the intention to quit (ITQ) among child welfare and protection (CWP) workers in Norway and its relationship with mentoring. Participants from 80 municipalities were surveyed at three time points (T1: <i>n</i> = 225, T2: <i>n</i> = 168, T3: <i>n</i> = 64). Linear mixed models revealed an increasing ITQ over time, with no significant impact of mentoring on ITQ trajectories or levels. Despite theoretical support for mentoring’s role in retention, variations in mentoring’s frequency, duration, and content may explain its lack of effect. The study suggests that future research should employ an experimental design to isolate the influence of specific mentoring attributes on CWP workers’ ITQ. Professional mentoring is proposed as a strategy to reduce turnover intentions.The term “mentoring” is frequently used interchangeably with guidance, coaching, and clinical or supportive supervision, varying by professional domain.The absence of a clear and universally accepted definition of mentoring leads to diverse practices and variations in both the content delivered and the qualifications of mentors.As currently implemented in Norwegian Child Welfare Services, mentoring is insufficient in addressing the increasing tendency of CWP workers to consider leaving their positions over time. Professional mentoring is proposed as a strategy to reduce turnover intentions. The term “mentoring” is frequently used interchangeably with guidance, coaching, and clinical or supportive supervision, varying by professional domain. The absence of a clear and universally accepted definition of mentoring leads to diverse practices and variations in both the content delivered and the qualifications of mentors. As currently implemented in Norwegian Child Welfare Services, mentoring is insufficient in addressing the increasing tendency of CWP workers to consider leaving their positions over time.
DOI: 10.5517/ccdc.csd.cc2hxpsx
title: CCDC 2321490: Experimental Crystal Structure Determination

description: Related Article: Shachendra Kumar Bharti, Keiko Odera, Kamini Tripathi, Benzamin D. Ward, S. Bhattacharya, Ryoya Takahashi, Lallan Mishra|2025|New J.Chem.|49|14219|doi:10.1039/D5NJ01491C
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccdc.csd.cc2m9v93
title: CCDC 2422535: Experimental Crystal Structure Determination

description: Related Article: Xiaolin Yuan, Zeping Chen, Chenghai Gao, Jianhua Ju, Xiangxi Yi, Qinglian Li|2025|Tetrahedron|186|134852|doi:10.1016/j.tet.2025.134852
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccdc.csd.cc2nb2fj
title: CCDC 2452547: Experimental Crystal Structure Determination

description: Related Article: Nubbemeyer, Udo, Schollmeyer, Dieter, Broy, Carina|2025|CSD Communication|||
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccdc.csd.cc2nb4cj
title: CCDC 2452607: Experimental Crystal Structure Determination

description: Related Article: Merzweiler, Kurt, Halz, Jan Henrik|2025|CSD Communication|||
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.5517/ccdc.csd.cc2nb58g
title: CCDC 2452635: Experimental Crystal Structure Determination

description: Related Article: Benedict Klinnert, Anne Jaeger|2025|CSD Communication|||
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.