gpt-oss-10.8b-specialized-science-pruned-moe-only-15-experts
11
1
10.8B
2 languages
license:apache-2.0
by
AmanPriyanshu
Language Model
OTHER
10.8B params
New
11 downloads
Early-stage
Edge AI:
Mobile
Laptop
Server
25GB+ RAM
Mobile
Laptop
Server
Quick Summary
AI model with specialized capabilities.
Device Compatibility
Mobile
4-6GB RAM
Laptop
16GB RAM
Server
GPU
Minimum Recommended
11GB+ RAM
Code Examples
Example 2text
<|channel|>analysis<|message|>Need explain greenhouse effect causes, mechanism.<|end|><|start|>assistant<|channel|>final<|message|>### What is the “greenhouse effect”?
The *greenhouse effect* (often called the *greenhouse‑green effect* or simply the *greenhouse effect*) is the phenomenon in which the atmosphere of Earth behaves like a greenhouse: it absorbs and re‑emises infrared (IR) radiation that is emitted by the Earth’s surface, keeping the surface warm. The effect is the net warming of the Earth’s surface that results from the atmosphere’s ability to trap heat.
---
## 1. Why the atmosphere is a greenhouse
| Property | Why it matters |
|----------|----------------|
| **Molecular composition** | The atmosphere is mainly H₂O, CO₂, N₂, O₂, and trace gases. These molecules have vibrational modes that absorb IR radiation. |
| **Optically thin in the visible** | In the visible part of the spectrum the atmosphere is largely transparent, so sunlight reaches the surface. |
| **Optically thick in the IR** | In the IR (≈ 0.7–5 µm) the atmosphere is opaque; photons emitted from the surface are repeatedly absorbed and re‑emitted. |
| **Long mean‑free‑path** | The IR photons travel a long distance before being absorbed, so the atmosphere behaves like a “black” body that re‑emises radiation. |
Because the Earth’s surface emits a lot of IR radiation (≈ 70 % of the solar energy it receives), the atmosphere’s ability to absorb and re‑emit that radiation keeps the surface warm.
---
## 2. How the greenhouse effect works
1. **Solar radiation reaches the surface**
The Sun’s spectrum peaks in the visible/near‑UV. The atmosphere is largely transparent to that radiation, so it reaches the surface and is absorbed by the Earth’s surface (mostly by the oceans and land).
2. **Surface emits IR radiation**
The surface, heated by the absorbed solar energy, emits a black‑body spectrum that peaks in the IR (≈ 10 µm). This IR radiation is the *thermal radiation* that the Earth would radiate if it were in space.
3. **Atmospheric absorption of IR**
As the IR photons travel upward, they encounter molecules that absorb at the same wavelengths. Each absorption event excites a molecule to a higher vibrational state.
4. **Re‑emExample 2text
<|channel|>analysis<|message|>Need explain greenhouse effect causes, mechanism.<|end|><|start|>assistant<|channel|>final<|message|>### What is the “greenhouse effect”?
The *greenhouse effect* (often called the *greenhouse‑green effect* or simply the *greenhouse effect*) is the phenomenon in which the atmosphere of Earth behaves like a greenhouse: it absorbs and re‑emises infrared (IR) radiation that is emitted by the Earth’s surface, keeping the surface warm. The effect is the net warming of the Earth’s surface that results from the atmosphere’s ability to trap heat.
---
## 1. Why the atmosphere is a greenhouse
| Property | Why it matters |
|----------|----------------|
| **Molecular composition** | The atmosphere is mainly H₂O, CO₂, N₂, O₂, and trace gases. These molecules have vibrational modes that absorb IR radiation. |
| **Optically thin in the visible** | In the visible part of the spectrum the atmosphere is largely transparent, so sunlight reaches the surface. |
| **Optically thick in the IR** | In the IR (≈ 0.7–5 µm) the atmosphere is opaque; photons emitted from the surface are repeatedly absorbed and re‑emitted. |
| **Long mean‑free‑path** | The IR photons travel a long distance before being absorbed, so the atmosphere behaves like a “black” body that re‑emises radiation. |
Because the Earth’s surface emits a lot of IR radiation (≈ 70 % of the solar energy it receives), the atmosphere’s ability to absorb and re‑emit that radiation keeps the surface warm.
---
## 2. How the greenhouse effect works
1. **Solar radiation reaches the surface**
The Sun’s spectrum peaks in the visible/near‑UV. The atmosphere is largely transparent to that radiation, so it reaches the surface and is absorbed by the Earth’s surface (mostly by the oceans and land).
2. **Surface emits IR radiation**
The surface, heated by the absorbed solar energy, emits a black‑body spectrum that peaks in the IR (≈ 10 µm). This IR radiation is the *thermal radiation* that the Earth would radiate if it were in space.
3. **Atmospheric absorption of IR**
As the IR photons travel upward, they encounter molecules that absorb at the same wavelengths. Each absorption event excites a molecule to a higher vibrational state.
4. **Re‑emExample 3text
<|channel|>analysis<|message|>Need to explain DNA structure: double helix, nucleotides, base pairing, major vs minor strands, sugar-phosphate backbone, base composition, major features. Function: genetic information, coding, replication, transcription, regulation, etc. Provide details.<|end|><|start|>assistant<|channel|>final<|message|>**DNA – the Double‑Helix of Life**
---
## 1. The Structure of DNA
| Feature | What It Is | Why It Matters |
|--------|-----------|----------------|
| **Double‑helix** | Two strands of a sugar‑phosphate backbone that wind around each other | Gives a rigid, stable scaffold that can be stretched, bent, and packed into the nucleus |
| **Backback** | 5‑carbon deoxyribose (or deoxoxylulose in RNA) + phosphate | Provides a “rail” for the bases; the phosphates are negatively charged, attracting Mg²⁺ ions that stabilize the helix |
| **Bases** | 4 nucleobases (A, T, C, G) | Carry the genetic code; each base is covalently attached to the sugar |
| **Base pairing** | Watson‑Crick model: A–T (purine–pyrimidine) and C–G (purine–purine) | Creates hydrogen‑bonded “stems” that lock the two strands together |
| **Major vs Minor strand** | The two strands are not identical; one is called the “major” (more bases) and the other the “minor” | The asymmetry gives a sense of direction for processes like replication and transcription |
| **Major groove** | The larger groove formed by the major strand | The enzyme machinery (polymerases, helicases) accesses the bases here |
| **Minor groove** | The smaller groove formed by the minor strand | Less accessible; often used for binding of proteins that need a tight fit |
| **Length** | 3.4 Å per base pair (≈ 0.34 nm) | Determines the spacing of bases; the helix completes every 10–10.5 bases |
| **Super‑structure** | DNA can form higher‑order structures: nucleosomes, loops, super‑loops, and higher‑order fibers | Enables compaction of the genome and regulation of gene expression |
### 1.1 The Sugar‑Phosphate Backbone
- **Phosphodiester linkage**: 3′‑phosphate of one sugar is covExample 3text
<|channel|>analysis<|message|>Need to explain DNA structure: double helix, nucleotides, base pairing, major vs minor strands, sugar-phosphate backbone, base composition, major features. Function: genetic information, coding, replication, transcription, regulation, etc. Provide details.<|end|><|start|>assistant<|channel|>final<|message|>**DNA – the Double‑Helix of Life**
---
## 1. The Structure of DNA
| Feature | What It Is | Why It Matters |
|--------|-----------|----------------|
| **Double‑helix** | Two strands of a sugar‑phosphate backbone that wind around each other | Gives a rigid, stable scaffold that can be stretched, bent, and packed into the nucleus |
| **Backback** | 5‑carbon deoxyribose (or deoxoxylulose in RNA) + phosphate | Provides a “rail” for the bases; the phosphates are negatively charged, attracting Mg²⁺ ions that stabilize the helix |
| **Bases** | 4 nucleobases (A, T, C, G) | Carry the genetic code; each base is covalently attached to the sugar |
| **Base pairing** | Watson‑Crick model: A–T (purine–pyrimidine) and C–G (purine–purine) | Creates hydrogen‑bonded “stems” that lock the two strands together |
| **Major vs Minor strand** | The two strands are not identical; one is called the “major” (more bases) and the other the “minor” | The asymmetry gives a sense of direction for processes like replication and transcription |
| **Major groove** | The larger groove formed by the major strand | The enzyme machinery (polymerases, helicases) accesses the bases here |
| **Minor groove** | The smaller groove formed by the minor strand | Less accessible; often used for binding of proteins that need a tight fit |
| **Length** | 3.4 Å per base pair (≈ 0.34 nm) | Determines the spacing of bases; the helix completes every 10–10.5 bases |
| **Super‑structure** | DNA can form higher‑order structures: nucleosomes, loops, super‑loops, and higher‑order fibers | Enables compaction of the genome and regulation of gene expression |
### 1.1 The Sugar‑Phosphate Backbone
- **Phosphodiester linkage**: 3′‑phosphate of one sugar is covDeploy This Model
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