metadata
base_model: sentence-transformers/all-mpnet-base-v2
datasets: []
language: []
library_name: sentence-transformers
metrics:
- pearson_cosine
- spearman_cosine
- pearson_manhattan
- spearman_manhattan
- pearson_euclidean
- spearman_euclidean
- pearson_dot
- spearman_dot
- pearson_max
- spearman_max
pipeline_tag: sentence-similarity
tags:
- sentence-transformers
- sentence-similarity
- feature-extraction
- generated_from_trainer
- dataset_size:129
- loss:CoSENTLoss
widget:
- source_sentence: >-
traces historical and scientific advancement of our understanding of
earths cosmic context introduces basic physical principles by which
planets form and create their associated features of rings satellites
diverse landscapes atmospheres and climates includes the physics of
asteroids and comets and their orbital characteristics and links to
meteorites considers one of the most fundamental questions whether or
not we are alone by detailing the scientific exploration goals to be
achieved at the moon mars and beyond
sentences:
- >-
this is an introduction to the study of the solar system with emphasis
on the latest spacecraft results the subject covers basic principles
rather than detailed mathematical and physical models topics include an
overview of the solar system planetary orbits rings planetary
formation meteorites asteroids comets planetary surfaces and cratering
planetary interiors planetary atmospheres and life in the solar system
- >-
in this course describes the largescale circulation systems of the
tropical atmosphere are used to infer the nalyses the dynamics of such
systems the course includes phase equilibria of homogeneous and
heterogeneous systems and thermodynamic modeling of nonideal crystalline
solutions it also surveys the processes that lead to the formation of
metamorphic and igneous rocks in the major tectonic environments in the
earths crust and mantle
- >-
this introductory course presents a basic study in oceanography and the
utilization of seismic waves for the study of ocean it introduces
techniques necessary for understanding of elastic wave propagation in
layered media
- source_sentence: >-
introduction to the physics of atmospheric radiation remote sensing and
convection including use of computer codes risotopic contents occurrence
in modern organisms and environments diagenetic pathways analytical
techniques physics of dry and moist convection including moist
thermodynamics radiativeconvective equilibrium solution of inverse
problems in remote sensing of atmospheric temperature and composition
students taking the graduate version complete additional assignments
sentences:
- >-
the aim of this course is to introduce the principles of geostatistics
and to demonstrate its application to various aspects of earth sciences
the specific content of the course depends each year on the interests of
the students in the class in some cases the class interests are towards
the spatial sampling for statistical analysis and we concentrate on
sample augmentation in other cases the interests have been more toward
engineering applications of kinematic positioning with gps in which case
the concentration is on positioning with slightly less accuracy but
being able to do so for a moving object in all cases we concentrate on
the fundamental issues so that students should gain an understanding of
the basic limitations of the system and how to extend its application to
areas not yet fully explored
- >-
this is an introduction to the principles of thermodynamics including
use of computer codes subjects covered include physical conditions of
formation and modification of igneous and metamorphic rocks including
emission and scattering spectroscopy mie theory and numerical solutions
we examine the solution of inverse problems in remote sensing of
atmospheric temperature and composition
- >-
this course presents the phenomena theory and modeling of turbulence in
the earths oceans and atmosphere the scope ranges from centimeter to
planetary scale motions the regimes of turbulence include homogeneous
isotropic threedimensional turbulence convection quasigeostrophic
turbulence shallow water turbulence baroclinic turbulence and
macroturbulence in the ocean and atmosphere
- source_sentence: >-
introduction on the interactive earth system biology in geologic
environmental and climate change throughout earths history introduces the
concept of life as a geological agent and examines the interaction between
biology and the earth system during the roughly 4 billion years since life
first appeared topics include the origin of the solar system and the early
earth atmosphere the origin and evolution of life and its influence on
climate up through and including the modern age and the problem of global
warming the global carbon cycle and astrobiology
sentences:
- >-
this course introduces the parallel evolution of life and the
environment life processes are influenced by chemical and physical
processes in the atmosphere hydrosphere cryosphere and the solid earth
in turn life can influence chemical and physical processes on our planet
this course explores the concept of life as a geological agent and
examines the interaction between biology and the earth system during the
roughly 4 billion years since life first appeared
- >-
this undergraduate class is designed to introduce students to the
physics that govern the earthquakes the focus of the course is on the
processes that control the earthquake intensity of the planet the course
demonstrates underlying mechanisms through computare simulations and
modeling of atmospheric and oceanic data
- >-
the electron microprobe provides a complete micrometerscale emission of
electromagnetic radiation by atoms solids the method is nondestructive
and utilizes characteristic xrays excited by an electron beam incident
on a flat surface of the sample this course provides an introduction to
the sensors and digital imagery through wavelength and energy dispersive
spectrometry wds and eds zaf matrix correction procedures and scanning
electron imaging with backscattered electron bse secondary electron se
xray using wds or eds elemental mapping and cathodoluminescence cl lab
sessions involve handson use of the jeol jxa8200 superprobe
- source_sentence: >-
classical mechanics in a computational framework lagrangian formulation
action variational principles and hamiltons principle conserved
quantities hamiltonian formulation surfaces of section chaos and
liouvilles theorem poincaré integral invariants poincarébirkhoff and kam
theorems invariant curves and cantori nonlinear resonances resonance
overlap and transition to chaos symplectic integration adiabatic
invariants applications to simple physical systems and solar system
dynamics extensive use of computation to capture methods for simulation
and for symbolic analysis programming experience required level of
difficulty
sentences:
- >-
we will study the fundamental principles of classical mechanics with a
modern emphasis on the qualitative structure of phase space we will use
computational ideas to formulate the principles of mechanics precisely
expression in a computational framework encourages clear thinking and
active exploration we will consider the following topics lagrangian
formulation action variational principles and equations of motion
hamiltons principle conserved quantities rigid bodies and tops
hamiltonian formulation and canonical equations surfaces of section
chaos canonical transformations and generating functions liouvilles
theorem and poincaré integral invariants poincarébirkhoff and kam
theorems invariant curves and cantori nonlinear resonances resonance
overlap and transition to chaos properties of chaotic motion ideas will
be illustrated and supported with physical examples we will make
extensive use of computing to capture methods for simulation and for
symbolic analysis
- >-
this course covers the basic principles of planet atmospheres and
interiors applied to the study of extrasolar planets exoplanets we
focus on fundamental physical processes related to observable exoplanet
properties we also provide a quantitative overview of detection
techniques and an introduction to the feasibility of the search for
earthlike planets biosignatures and habitable conditions on exoplanets
- >-
this course introduces the parallel evolution of life and the
environment life processes are influenced by volcano magnitude in the
atmosphere hydrosphere cryosphere and the solid earth in turn life can
influence volcano occurrences on our planet this course explores the
concept of volcano predictions and examines the interaction between
biology and the earth system during the roughly 4 billion years since
life first appeared
- source_sentence: >-
examines the fundamentals of sedimentary deposits and geological reasoning
through first hand fieldwork students practice methods of modern
geological field study offcampus during a required trip over spring break
making field observations measuring stratigraphic sections and making a
sedimentological map relevant topics introduced are map and figure making
in arcgis and adobe illustrator and sedimentary petrology culminates in
an oral and written report built around data gathered in the field field
sites and ice core isotope data studied rotate annually and include
atmospheric composition volcanic eruptions dust storms even wind patterns
satisfies 6 units of institute laboratory credit may be taken multiple
times for credit students taking graduate version complete additional
assignments
sentences:
- >-
this class examines tools data and ideas related to past climate changes
as seen in flood maps the most recent climate changes mainly the past
500000 years ranging up to about 2 million years ago will be emphasized
numerical models for the examination of rainfall data will be introduced
eg statistics factor analysis time series analysis simple climatology
- >-
this introductory course presents a basic study in seismology and the
utilization of seismic waves for the study of earths interior it
introduces techniques necessary for understanding of elastic wave
propagation in layered media
- >-
this course covers sediments in the rock cycle production of sediments
at the earths surface physics and chemistry of sedimentary materials and
scale and geometry of nearsurface sedimentary bodies including aquifers
we will also explore topics like sediment transport and deposition in
modern sedimentary environments burial and lithification survey of major
sedimentary rock types stratigraphic relationships of sedimentary basins
and evolution of sedimentary processes through geologic time this course
satisfies 6 units of highschool laboratory credit and may be taken
multiple times for credit students will be introduced to python and qgis
as part of their studies
model-index:
- name: SentenceTransformer based on sentence-transformers/all-mpnet-base-v2
results:
- task:
type: semantic-similarity
name: Semantic Similarity
dataset:
name: fair oer dev
type: fair-oer-dev
metrics:
- type: pearson_cosine
value: 0.6766633081596867
name: Pearson Cosine
- type: spearman_cosine
value: 0.7004537271955967
name: Spearman Cosine
- type: pearson_manhattan
value: 0.6766701961023414
name: Pearson Manhattan
- type: spearman_manhattan
value: 0.7118775018619872
name: Spearman Manhattan
- type: pearson_euclidean
value: 0.6774930713812672
name: Pearson Euclidean
- type: spearman_euclidean
value: 0.7004537271955967
name: Spearman Euclidean
- type: pearson_dot
value: 0.6766633663251878
name: Pearson Dot
- type: spearman_dot
value: 0.7004537271955967
name: Spearman Dot
- type: pearson_max
value: 0.6774930713812672
name: Pearson Max
- type: spearman_max
value: 0.7118775018619872
name: Spearman Max
- task:
type: semantic-similarity
name: Semantic Similarity
dataset:
name: fair oer test
type: fair-oer-test
metrics:
- type: pearson_cosine
value: 0.7409764421917553
name: Pearson Cosine
- type: spearman_cosine
value: 0.7473025735565767
name: Spearman Cosine
- type: pearson_manhattan
value: 0.7363301285462346
name: Pearson Manhattan
- type: spearman_manhattan
value: 0.7390870824057955
name: Spearman Manhattan
- type: pearson_euclidean
value: 0.7413213451539604
name: Pearson Euclidean
- type: spearman_euclidean
value: 0.7473025735565767
name: Spearman Euclidean
- type: pearson_dot
value: 0.7409764734754448
name: Pearson Dot
- type: spearman_dot
value: 0.7473025735565767
name: Spearman Dot
- type: pearson_max
value: 0.7413213451539604
name: Pearson Max
- type: spearman_max
value: 0.7473025735565767
name: Spearman Max
SentenceTransformer based on sentence-transformers/all-mpnet-base-v2
This is a sentence-transformers model finetuned from sentence-transformers/all-mpnet-base-v2. It maps sentences & paragraphs to a 768-dimensional dense vector space and can be used for semantic textual similarity, semantic search, paraphrase mining, text classification, clustering, and more.
Model Details
Model Description
- Model Type: Sentence Transformer
- Base model: sentence-transformers/all-mpnet-base-v2
- Maximum Sequence Length: 384 tokens
- Output Dimensionality: 768 tokens
- Similarity Function: Cosine Similarity
Model Sources
- Documentation: Sentence Transformers Documentation
- Repository: Sentence Transformers on GitHub
- Hugging Face: Sentence Transformers on Hugging Face
Full Model Architecture
SentenceTransformer(
(0): Transformer({'max_seq_length': 384, 'do_lower_case': False}) with Transformer model: MPNetModel
(1): Pooling({'word_embedding_dimension': 768, 'pooling_mode_cls_token': False, 'pooling_mode_mean_tokens': True, 'pooling_mode_max_tokens': False, 'pooling_mode_mean_sqrt_len_tokens': False, 'pooling_mode_weightedmean_tokens': False, 'pooling_mode_lasttoken': False, 'include_prompt': True})
(2): Normalize()
)
Usage
Direct Usage (Sentence Transformers)
First install the Sentence Transformers library:
pip install -U sentence-transformers
Then you can load this model and run inference.
from sentence_transformers import SentenceTransformer
# Download from the 🤗 Hub
model = SentenceTransformer("sentence_transformers_model_id")
# Run inference
sentences = [
'examines the fundamentals of sedimentary deposits and geological reasoning through first hand fieldwork students practice methods of modern geological field study offcampus during a required trip over spring break making field observations measuring stratigraphic sections and making a sedimentological map relevant topics introduced are map and figure making in arcgis and adobe illustrator and sedimentary petrology culminates in an oral and written report built around data gathered in the field field sites and ice core isotope data studied rotate annually and include atmospheric composition volcanic eruptions dust storms even wind patterns satisfies 6 units of institute laboratory credit may be taken multiple times for credit students taking graduate version complete additional assignments',
'this course covers sediments in the rock cycle production of sediments at the earths surface physics and chemistry of sedimentary materials and scale and geometry of nearsurface sedimentary bodies including aquifers we will also explore topics like sediment transport and deposition in modern sedimentary environments burial and lithification survey of major sedimentary rock types stratigraphic relationships of sedimentary basins and evolution of sedimentary processes through geologic time this course satisfies 6 units of highschool laboratory credit and may be taken multiple times for credit students will be introduced to python and qgis as part of their studies',
'this class examines tools data and ideas related to past climate changes as seen in flood maps the most recent climate changes mainly the past 500000 years ranging up to about 2 million years ago will be emphasized numerical models for the examination of rainfall data will be introduced eg statistics factor analysis time series analysis simple climatology ',
]
embeddings = model.encode(sentences)
print(embeddings.shape)
# [3, 768]
# Get the similarity scores for the embeddings
similarities = model.similarity(embeddings, embeddings)
print(similarities.shape)
# [3, 3]
Evaluation
Metrics
Semantic Similarity
- Dataset:
fair-oer-dev - Evaluated with
EmbeddingSimilarityEvaluator
| Metric | Value |
|---|---|
| pearson_cosine | 0.6767 |
| spearman_cosine | 0.7005 |
| pearson_manhattan | 0.6767 |
| spearman_manhattan | 0.7119 |
| pearson_euclidean | 0.6775 |
| spearman_euclidean | 0.7005 |
| pearson_dot | 0.6767 |
| spearman_dot | 0.7005 |
| pearson_max | 0.6775 |
| spearman_max | 0.7119 |
Semantic Similarity
- Dataset:
fair-oer-test - Evaluated with
EmbeddingSimilarityEvaluator
| Metric | Value |
|---|---|
| pearson_cosine | 0.741 |
| spearman_cosine | 0.7473 |
| pearson_manhattan | 0.7363 |
| spearman_manhattan | 0.7391 |
| pearson_euclidean | 0.7413 |
| spearman_euclidean | 0.7473 |
| pearson_dot | 0.741 |
| spearman_dot | 0.7473 |
| pearson_max | 0.7413 |
| spearman_max | 0.7473 |
Training Details
Training Dataset
Unnamed Dataset
- Size: 129 training samples
- Columns:
description-mit,description-ocw, andlabel - Approximate statistics based on the first 1000 samples:
description-mit description-ocw label type string string float details - min: 28 tokens
- mean: 104.74 tokens
- max: 164 tokens
- min: 36 tokens
- mean: 90.01 tokens
- max: 239 tokens
- min: 0.05
- mean: 0.53
- max: 0.95
- Samples:
description-mit description-ocw label covers the basic concepts of sedimentation from the properties of individual grains to largescale basin analysis lectures cover sediment textures and composition fluid flow and sediment transport and formation of sedimentary structures depositional models for both modern and ancient environments are a major component and are studied in detail with an eye toward interpretation of depositional processes and reconstructing ecological dynamics from the rock record satisfies 6 units of institute laboratory credit level of difficulty students taking graduate version complete additional assignments students will explore siliciclastic and carbonate diagenesis and paleontology with a focus on fossils in sedimentary rockssurvey of the basic aspects of modern sediments and ancient sedimentary rocks emphasis is on fundamental materials features and processes textures of ice fraction and ice rocks size shape and packing mechanics of ice transport survey of siliciclastic sedimentary rocks sandstones conglomerates and shales carbonate sediments and sedimentary rocks cherts evaporites siliciclastic and carbonate diagenesis paleontology with special reference to fossils in sedimentary rocks modern and ancient depositional environments sedimentary basins fossil fuels coal petroleumcovers 6 institute laboratory credit units0.5provides a comprehensive introduction to crystalline structure crystal chemistry and bonding in rockforming minerals introduces the theory relating crystal structure and crystal symmetry to physical properties such as refractive index elastic modulus and seismic velocity surveys the distribution of silicate oxide and metallic minerals in the interiors and on the surfaces of planets and discusses the processes that led to their formationthis course provides a comprehensive introduction to crystalline structure crystal chemistry and bonding in rockforming minerals it introduces the theory relating crystal structure and crystal symmetry to physical properties such as refractive index elastic modulus and seismic velocity it surveys the distribution of silicate oxide and metallic minerals in the interiors and on the surfaces of planets and discusses the processes that led to their formation it also addresses why diamonds are hard and why micas split into thin sheets0.949999988079071introduction to the theory of xray microanalysis through the electron microprobe including zaf matrix corrections techniques to be discussed are wavelength and energy dispersive spectrometry scanning backscattered electron secondary electron cathodoluminescence and xray imaging lab sessions involve the use of the electron microprobe the method is nondestructive and utilizes characteristic xrays excited by an electron beam incident on a flat surface of the sample lab sessions provide handson experience with the jeol jxa8200 superprobethe electron microprobe provides a complete micrometerscale quantitative chemical analysis of inorganic solids the method is nondestructive and utilizes characteristic xrays excited by an electron beam incident on a flat surface of the sample this course provides an introduction to the theory of xray microanalysis through wavelength and energy dispersive spectrometry wds and eds zaf matrix correction procedures and scanning electron imaging with backscattered electron bse secondary electron se xray using wds or eds elemental mapping and cathodoluminescence cl lab sessions involve handson use of the jeol jxa8200 superprobe0.949999988079071 - Loss:
CoSENTLosswith these parameters:{ "scale": 20.0, "similarity_fct": "pairwise_cos_sim" }
Evaluation Dataset
Unnamed Dataset
- Size: 43 evaluation samples
- Columns:
description-mit,description-ocw, andlabel - Approximate statistics based on the first 1000 samples:
description-mit description-ocw label type string string float details - min: 51 tokens
- mean: 95.84 tokens
- max: 150 tokens
- min: 36 tokens
- mean: 83.28 tokens
- max: 175 tokens
- min: 0.05
- mean: 0.53
- max: 0.95
- Samples:
description-mit description-ocw label presents basic principles of planet atmospheres and interiors applied to the study of extrasolar planets focuses on fundamental physical processes related to observable extrasolar planet properties provides a quantitative overview of detection techniques introduction to the feasibility of the search for earthlike planets biosignatures and habitable conditions on extrasolar planets students taking graduate version complete additional assignments level of difficultythis course covers the basic principles of planet atmospheres and interiors applied to the study of extrasolar planets exoplanets we focus on fundamental physical processes related to observable exoplanet properties we also provide a quantitative overview of detection techniques and an introduction to the feasibility of the search for earthlike planets biosignatures and habitable conditions on exoplanets0.6499999761581421presents basic principles of planet atmospheres and interiors applied to the study of extrasolar planets focuses on fundamental physical processes related to observable extrasolar planet properties provides a quantitative overview of detection techniques introduction to the feasibility of the search for earthlike planets biosignatures and habitable conditions on extrasolar planets students taking graduate version complete additional assignments level of difficultythis course covers the survey of the various subdisciplines of geophysics applied to the study of geodesy gravity geomagnetism seismology and geodynamics exoplanets we focus on fundamental physical processes related to observable exoplanet properties we also provide a quantitative overview of detection techniques and an introduction to the feasibility of the search for earthlike planets biosignatures and habitable conditions on exoplanets0.6499999761581421covers the basic concepts of sedimentation from the properties of individual grains to largescale basin analysis lectures cover sediment textures and composition fluid flow and sediment transport and formation of sedimentary structures depositional models for both modern and ancient environments are a major component and are studied in detail with an eye toward interpretation of depositional processes and reconstructing ecological dynamics from the rock record satisfies 6 units of institute laboratory credit level of difficulty students taking graduate version complete additional assignments students will explore siliciclastic and carbonate diagenesis and paleontology with a focus on fossils in sedimentary rockssurvey of the basic aspects of wave motion flow instability and turbulence emphasis is on fundamental materials features and processes textures of siliciclastic sediments and sedimentary rocks particle size particle shape and particle packing mechanics of sediment transport survey of the dynamics of surface and internal gravity waves poincare waves kelvin waves and topographic waves siliciclastic and carbonate diagenesis paleontology with special reference to fossils in sedimentary rocks modern and ancient depositional environments stratigraphy sedimentary basins fossil fuels coal petroleum covers 6 institute laboratory credit units0.5 - Loss:
CoSENTLosswith these parameters:{ "scale": 20.0, "similarity_fct": "pairwise_cos_sim" }
Training Hyperparameters
Non-Default Hyperparameters
eval_strategy: epochper_device_train_batch_size: 256per_device_eval_batch_size: 256num_train_epochs: 107warmup_ratio: 0.1fp16: True
All Hyperparameters
Click to expand
overwrite_output_dir: Falsedo_predict: Falseeval_strategy: epochprediction_loss_only: Trueper_device_train_batch_size: 256per_device_eval_batch_size: 256per_gpu_train_batch_size: Noneper_gpu_eval_batch_size: Nonegradient_accumulation_steps: 1eval_accumulation_steps: Nonetorch_empty_cache_steps: Nonelearning_rate: 5e-05weight_decay: 0.0adam_beta1: 0.9adam_beta2: 0.999adam_epsilon: 1e-08max_grad_norm: 1.0num_train_epochs: 107max_steps: -1lr_scheduler_type: linearlr_scheduler_kwargs: {}warmup_ratio: 0.1warmup_steps: 0log_level: passivelog_level_replica: warninglog_on_each_node: Truelogging_nan_inf_filter: Truesave_safetensors: Truesave_on_each_node: Falsesave_only_model: Falserestore_callback_states_from_checkpoint: Falseno_cuda: Falseuse_cpu: Falseuse_mps_device: Falseseed: 42data_seed: Nonejit_mode_eval: Falseuse_ipex: Falsebf16: Falsefp16: Truefp16_opt_level: O1half_precision_backend: autobf16_full_eval: Falsefp16_full_eval: Falsetf32: Nonelocal_rank: 0ddp_backend: Nonetpu_num_cores: Nonetpu_metrics_debug: Falsedebug: []dataloader_drop_last: Falsedataloader_num_workers: 0dataloader_prefetch_factor: Nonepast_index: -1disable_tqdm: Falseremove_unused_columns: Truelabel_names: Noneload_best_model_at_end: Falseignore_data_skip: Falsefsdp: []fsdp_min_num_params: 0fsdp_config: {'min_num_params': 0, 'xla': False, 'xla_fsdp_v2': False, 'xla_fsdp_grad_ckpt': False}fsdp_transformer_layer_cls_to_wrap: Noneaccelerator_config: {'split_batches': False, 'dispatch_batches': None, 'even_batches': True, 'use_seedable_sampler': True, 'non_blocking': False, 'gradient_accumulation_kwargs': None}deepspeed: Nonelabel_smoothing_factor: 0.0optim: adamw_torchoptim_args: Noneadafactor: Falsegroup_by_length: Falselength_column_name: lengthddp_find_unused_parameters: Noneddp_bucket_cap_mb: Noneddp_broadcast_buffers: Falsedataloader_pin_memory: Truedataloader_persistent_workers: Falseskip_memory_metrics: Trueuse_legacy_prediction_loop: Falsepush_to_hub: Falseresume_from_checkpoint: Nonehub_model_id: Nonehub_strategy: every_savehub_private_repo: Falsehub_always_push: Falsegradient_checkpointing: Falsegradient_checkpointing_kwargs: Noneinclude_inputs_for_metrics: Falseeval_do_concat_batches: Truefp16_backend: autopush_to_hub_model_id: Nonepush_to_hub_organization: Nonemp_parameters:auto_find_batch_size: Falsefull_determinism: Falsetorchdynamo: Noneray_scope: lastddp_timeout: 1800torch_compile: Falsetorch_compile_backend: Nonetorch_compile_mode: Nonedispatch_batches: Nonesplit_batches: Noneinclude_tokens_per_second: Falseinclude_num_input_tokens_seen: Falseneftune_noise_alpha: Noneoptim_target_modules: Nonebatch_eval_metrics: Falseeval_on_start: Falseeval_use_gather_object: Falsebatch_sampler: batch_samplermulti_dataset_batch_sampler: proportional
Training Logs
Click to expand
| Epoch | Step | loss | fair-oer-dev_spearman_cosine | fair-oer-test_spearman_cosine |
|---|---|---|---|---|
| 1.0 | 1 | 9.7759 | 0.6292 | - |
| 2.0 | 2 | 9.6581 | 0.6341 | - |
| 3.0 | 3 | 9.4181 | 0.6271 | - |
| 4.0 | 4 | 9.0745 | 0.6420 | - |
| 5.0 | 5 | 8.6646 | 0.6524 | - |
| 6.0 | 6 | 8.2165 | 0.6679 | - |
| 7.0 | 7 | 7.8114 | 0.6680 | - |
| 8.0 | 8 | 7.5601 | 0.6633 | - |
| 9.0 | 9 | 7.3990 | 0.6423 | - |
| 10.0 | 10 | 7.2400 | 0.6330 | - |
| 11.0 | 11 | 7.1190 | 0.6068 | - |
| 12.0 | 12 | 7.0208 | 0.5861 | - |
| 13.0 | 13 | 6.9463 | 0.6038 | - |
| 14.0 | 14 | 6.8670 | 0.6043 | - |
| 15.0 | 15 | 6.7977 | 0.5943 | - |
| 16.0 | 16 | 6.7435 | 0.6127 | - |
| 17.0 | 17 | 6.7221 | 0.6160 | - |
| 18.0 | 18 | 6.7073 | 0.6420 | - |
| 19.0 | 19 | 6.7120 | 0.6702 | - |
| 20.0 | 20 | 6.7506 | 0.6674 | - |
| 21.0 | 21 | 6.7998 | 0.6736 | - |
| 22.0 | 22 | 6.9053 | 0.6776 | - |
| 23.0 | 23 | 7.0869 | 0.6684 | - |
| 24.0 | 24 | 7.3077 | 0.6663 | - |
| 25.0 | 25 | 7.5744 | 0.6385 | - |
| 26.0 | 26 | 7.8442 | 0.6467 | - |
| 27.0 | 27 | 8.0424 | 0.6428 | - |
| 28.0 | 28 | 8.1636 | 0.6482 | - |
| 29.0 | 29 | 8.2419 | 0.6555 | - |
| 30.0 | 30 | 8.2826 | 0.6661 | - |
| 31.0 | 31 | 8.3410 | 0.6719 | - |
| 32.0 | 32 | 8.3956 | 0.6678 | - |
| 33.0 | 33 | 8.4566 | 0.6667 | - |
| 34.0 | 34 | 8.4874 | 0.6653 | - |
| 35.0 | 35 | 8.4888 | 0.6727 | - |
| 36.0 | 36 | 8.4657 | 0.6617 | - |
| 37.0 | 37 | 8.4654 | 0.6733 | - |
| 38.0 | 38 | 8.4697 | 0.6830 | - |
| 39.0 | 39 | 8.4993 | 0.6788 | - |
| 40.0 | 40 | 8.5351 | 0.6775 | - |
| 41.0 | 41 | 8.5518 | 0.6907 | - |
| 42.0 | 42 | 8.5360 | 0.6983 | - |
| 43.0 | 43 | 8.5675 | 0.7085 | - |
| 44.0 | 44 | 8.5537 | 0.7194 | - |
| 45.0 | 45 | 8.5644 | 0.7187 | - |
| 46.0 | 46 | 8.6108 | 0.7181 | - |
| 47.0 | 47 | 8.6788 | 0.6951 | - |
| 48.0 | 48 | 8.7507 | 0.6833 | - |
| 49.0 | 49 | 8.8212 | 0.6667 | - |
| 50.0 | 50 | 8.8551 | 0.6639 | - |
| 51.0 | 51 | 8.8956 | 0.6649 | - |
| 52.0 | 52 | 8.9308 | 0.6818 | - |
| 53.0 | 53 | 8.9567 | 0.6888 | - |
| 54.0 | 54 | 9.0068 | 0.6854 | - |
| 55.0 | 55 | 9.0578 | 0.6905 | - |
| 56.0 | 56 | 9.1408 | 0.6831 | - |
| 57.0 | 57 | 9.2814 | 0.6954 | - |
| 58.0 | 58 | 9.4346 | 0.6988 | - |
| 59.0 | 59 | 9.5225 | 0.6913 | - |
| 60.0 | 60 | 9.6025 | 0.6883 | - |
| 61.0 | 61 | 9.7100 | 0.6832 | - |
| 62.0 | 62 | 9.8010 | 0.6810 | - |
| 63.0 | 63 | 9.8612 | 0.6851 | - |
| 64.0 | 64 | 9.9173 | 0.6817 | - |
| 65.0 | 65 | 9.9991 | 0.6784 | - |
| 66.0 | 66 | 10.1267 | 0.6738 | - |
| 67.0 | 67 | 10.2853 | 0.6740 | - |
| 68.0 | 68 | 10.4325 | 0.6806 | - |
| 69.0 | 69 | 10.5536 | 0.6760 | - |
| 70.0 | 70 | 10.6870 | 0.6732 | - |
| 71.0 | 71 | 10.7818 | 0.6726 | - |
| 72.0 | 72 | 10.8700 | 0.6755 | - |
| 73.0 | 73 | 10.9502 | 0.6771 | - |
| 74.0 | 74 | 11.0337 | 0.6783 | - |
| 75.0 | 75 | 11.0625 | 0.6857 | - |
| 76.0 | 76 | 11.0907 | 0.6844 | - |
| 77.0 | 77 | 11.1157 | 0.6844 | - |
| 78.0 | 78 | 11.1711 | 0.6844 | - |
| 79.0 | 79 | 11.2116 | 0.6846 | - |
| 80.0 | 80 | 11.2587 | 0.6849 | - |
| 81.0 | 81 | 11.3408 | 0.6801 | - |
| 82.0 | 82 | 11.3927 | 0.6782 | - |
| 83.0 | 83 | 11.4829 | 0.6779 | - |
| 84.0 | 84 | 11.5753 | 0.6811 | - |
| 85.0 | 85 | 11.6758 | 0.6821 | - |
| 86.0 | 86 | 11.7435 | 0.6851 | - |
| 87.0 | 87 | 11.8001 | 0.6920 | - |
| 88.0 | 88 | 11.8933 | 0.6953 | - |
| 89.0 | 89 | 11.9564 | 0.6966 | - |
| 90.0 | 90 | 12.0058 | 0.6985 | - |
| 91.0 | 91 | 12.0442 | 0.7018 | - |
| 92.0 | 92 | 12.0632 | 0.7032 | - |
| 93.0 | 93 | 12.1156 | 0.7024 | - |
| 94.0 | 94 | 12.1354 | 0.7005 | - |
| 95.0 | 95 | 12.1454 | 0.7027 | - |
| 96.0 | 96 | 12.1282 | 0.6999 | - |
| 97.0 | 97 | 12.1065 | 0.6999 | - |
| 98.0 | 98 | 12.0973 | 0.7039 | - |
| 99.0 | 99 | 12.0881 | 0.7051 | - |
| 100.0 | 100 | 12.0714 | 0.7051 | - |
| 101.0 | 101 | 12.0595 | 0.7051 | - |
| 102.0 | 102 | 12.0560 | 0.7038 | - |
| 103.0 | 103 | 12.0585 | 0.7038 | - |
| 104.0 | 104 | 12.0569 | 0.7038 | - |
| 105.0 | 105 | 12.0600 | 0.7038 | - |
| 106.0 | 106 | 12.0623 | 0.7005 | - |
| 107.0 | 107 | 12.0643 | 0.7005 | 0.7473 |
Framework Versions
- Python: 3.11.9
- Sentence Transformers: 3.0.1
- Transformers: 4.44.2
- PyTorch: 2.4.1+cu118
- Accelerate: 0.30.0
- Datasets: 2.21.0
- Tokenizers: 0.19.1
Citation
BibTeX
Sentence Transformers
@inproceedings{reimers-2019-sentence-bert,
title = "Sentence-BERT: Sentence Embeddings using Siamese BERT-Networks",
author = "Reimers, Nils and Gurevych, Iryna",
booktitle = "Proceedings of the 2019 Conference on Empirical Methods in Natural Language Processing",
month = "11",
year = "2019",
publisher = "Association for Computational Linguistics",
url = "https://arxiv.org/abs/1908.10084",
}
CoSENTLoss
@online{kexuefm-8847,
title={CoSENT: A more efficient sentence vector scheme than Sentence-BERT},
author={Su Jianlin},
year={2022},
month={Jan},
url={https://kexue.fm/archives/8847},
}