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Related Concept Videos

Precipitation Processes01:12

Precipitation Processes

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The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
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Precipitation and Co-precipitation01:17

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Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
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Precipitation Gravimetry01:03

Precipitation Gravimetry

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Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
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Boundary Layer Characteristics01:18

Boundary Layer Characteristics

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When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
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Responses to Drought and Flooding02:41

Responses to Drought and Flooding

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Water plays a significant role in the life cycle of plants. However, insufficient or excess of water can be detrimental and pose a serious threat to plants.
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Related Experiment Video

Updated: Sep 15, 2025

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
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Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

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Meteorological drought severity forecasting utilizing blended modelling.

Aaditya Ahire1, Nilima Zade1, Umeed Mujawar1

  • 1Symbiosis Institute of Technology, Pune Campus, Symbiosis International (Deemed University), Pune 412115, Maharashtra, India.

Methodsx
|July 18, 2025
PubMed
Summary
This summary is machine-generated.

Accurate drought forecasting is crucial due to climate change. An ensemble model combining Extreme Gradient Boosting (XGBoost), Long Short Term Memory (LSTM), and TabNet significantly improves prediction accuracy over traditional methods.

Keywords:
Deep Learning Approach to Forecast Drought SeverityDrought prediction, Ensemble modelLSTMRMSETabNetXGBoost

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Watershed Planning within a Quantitative Scenario Analysis Framework
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Related Experiment Videos

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Watershed Planning within a Quantitative Scenario Analysis Framework
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Area of Science:

  • Environmental Science
  • Data Science
  • Meteorology

Background:

  • Droughts are increasing in frequency and intensity due to climate variation, causing significant damage to ecosystems, agriculture, and water resources.
  • Conventional drought forecasting methods struggle with complex time-space correlations in meteorological data.
  • Accurate drought prediction is imperative for effective disaster management and resource planning.

Purpose of the Study:

  • To develop a highly accurate drought forecasting model by integrating advanced machine learning techniques.
  • To leverage the strengths of Extreme Gradient Boosting (XGBoost), Long Short Term Memory (LSTM), and Tabular Network (TabNet) for improved drought severity prediction.

Main Methods:

  • An ensemble model was created by combining XGBoost for feature selection, LSTM for temporal pattern analysis, and TabNet for attention-based insights.
  • The model utilized a large meteorological dataset including temperature, precipitation, humidity, and wind speed.
  • Performance was evaluated using metrics such as Root Mean Square Error (RMSE), Mean Absolute Error (MAE), Coefficient of Determination (R²), Nash-Sutcliffe Efficiency (NSE), and Kling-Gupta Efficiency (KGE).

Main Results:

  • The proposed ensemble model demonstrated superior performance compared to individual models.
  • Achieved the lowest RMSE (0.6582) and MAE (0.5377), and the highest R² (0.5069).
  • Yielded the best NSE (0.5107) and KGE (0.6039), confirming its effectiveness in drought severity forecasting.

Conclusions:

  • The ensemble model significantly outperforms traditional methods in drought forecasting.
  • This advanced approach aids in providing early drought warnings and supports water conservation planning.
  • The integration of XGBoost, LSTM, and TabNet offers a robust solution for predicting drought severity.