Initial commit

.claude-plugin/plugin.json

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+{
+  "name": "Typst",
+  "description": "Typst文档编写SKILLS",
+  "version": "0.0.0-2025.11.28",
+  "author": {
+    "name": "Dongdong Kong",
+    "email": "kongdd.sysu@gmail.com"
+  },
+  "skills": [
+    "./skills/typst-physica"
+  ]
+}

README.md

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+# Typst
+
+Typst文档编写SKILLS

plugin.lock.json

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+{
+  "$schema": "internal://schemas/plugin.lock.v1.json",
+  "pluginId": "gh:kongdd/Skills_for_Your_AI_Student:typst",
+  "normalized": {
+    "repo": null,
+    "ref": "refs/tags/v20251128.0",
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+    "treeHash": "1011e000ccdd74ff53760c9de415719cbec5b2bca9b552608410d20458335269",
+    "generatedAt": "2025-11-28T10:19:56.227560Z",
+    "toolVersion": "publish_plugins.py@0.2.0"
+  },
+  "origin": {
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+    "branch": "master",
+    "commit": "aa1497ed0949fd50e99e70d6324a29c5b34f9390",
+    "repoRoot": "/Users/zhongweili/projects/openmind/42plugin-data"
+  },
+  "manifest": {
+    "name": "Typst",
+    "description": "Typst文档编写SKILLS"
+  },
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+    "files": [
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+        "path": "README.md",
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+        "sha256": "57ed3996ea71bb92281480cf2089cb385ab53dc7203e55913e7f348936c177d6"
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+      {
+        "path": "skills/typst-physica/examples.typ",
+        "sha256": "f29c070d485af884731333a127b9933966faee31d5682c9e77858b93a1822853"
+      },
+      {
+        "path": "skills/typst-physica/example_physica.typ",
+        "sha256": "a3aeff09aa965d57419261a9a3d9a206652c5b730c1f59afe7c6eb33a1b66bf9"
+      },
+      {
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+      }
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+  },
+  "security": {
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+    "scannerVersion": null,
+    "flags": []
+  }
+}

skills/typst-physica/SKILL.md

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+---
+name: typst-physica
+description: typst公式中的微分、偏微分方程编写，latex公式转typst。
+---
+
+
+# 引用包
+
+应在typst文档的开头，引用包。公式编写、文档排版，依赖`modern-cug-report`。
+
+用于如果已经引用了`modern-cug-report`，则无需再重复添加了。
+
+```typst
+#import "@local/modern-cug-report:0.1.3": *
+#show: doc => template(doc, footer: "CUG水文气象学2025", header: "")
+```
+
+
+# 偏微分方程
+
+- `(∂ theta) / (∂ t)`
+
+  `\frac{\partial \theta}{\partial t}`采用typst编写会非常简单，`pdv(theta, t)`
+
+  ```typst
+  (partial.diff theta) / (partial.diff t) // 是错误写法
+  pdv(theta, t)                           // 正确写法
+  ```
+
+- `(d theta) / (d t)`则是：`dv(theta, t)`
+
+
+# text
+
+typst公式中的本文需要使用引号：
+
+```typst
+q_(infiltration)   // 错误
+q_("infiltration") // 正确
+```
+
+# fraction
+
+- latex的`\frac{y}{x}`，写成typst则是`y/x`；
+  
+  若分子、分母有多个变量，则用括号括起来。例如latex的`\frac{y z}{x}`，写成typst则是`(y z) / x`
+
+
+# 排版
+
+- 一级标题之前空两行，凸显章节的层次感。
+
+- 第一个一级标题，不用空两行。

skills/typst-physica/example_physica.typ

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+// Copyright 2023 Leedehai
+// Use of this code is governed by a MIT license in the LICENSE.txt file.
+// For a manual on this package, see physica-manual.pdf.
+
+#import "@local/modern-cug-report:0.1.3": *
+#show: doc => template(doc, footer: "CUG水文气象学2025", header: "")
+
+// #import "physica.typ": *
+
+#show: super-T-as-transpose // Render "..^T" as transposed matrix
+
+$
+  A^T, curl vb(E) = - pdv(vb(B), t),
+  quad
+  tensor(Lambda, +mu, -nu) = dmat(1, RR),
+  quad
+  f(x,y) dd(x, y),
+  quad
+  dd(vb(x), y, [3]),
+  quad
+  dd(x, y, 2, d: Delta, p: and),
+  quad
+  dv(phi, t, d: upright(D)) = pdv(phi, t) + vb(u) grad phi \
+  H(f) = hmat(f; x, y; delim: "[", big: #true),
+  quad
+  vb(v^a) = sum_(i=1)^n alpha_i vu(u^i),
+  quad
+  Set((x, y), pdv(f, x, y, [2,1]) + pdv(f, x, y, [1,2]) < epsilon) \
+  -1/c^2 pdv(, t, 2)psi + laplacian psi = (m^2c^2) / hbar^2 psi,
+  quad
+  ket(n^((1))) = sum_(k in.not D) mel(k^((0)), V, n^((0))) / (E_n^((0)) - E_k^((0))) ket(k^((0))),
+  quad
+  integral_V dd(V) (pdv(cal(L), phi) - partial_mu (pdv(cal(L), (partial_mu phi)))) = 0 \
+  dd(s, 2) = -(1-(2G M)/r) dd(t, 2) + (1-(2G M)/r)^(-1) dd(r, 2) + r^2 dd(Omega, 2)
+$
+
+$
+  "clk:" & signals("|1....|0....|1....|0....|1....|0....|1....|0..", step: #0.5em) \
+  "bus:" & signals(" #.... X=... ..... ..... X=... ..... ..... X#.", step: #0.5em)
+$

skills/typst-physica/examples.typ

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+#import "@local/modern-cug-report:0.1.3": *
+#show: doc => template(doc, footer: "CUG水文气象学2025", header: "")
+
+
+== 1 Richards方程
+
+Richards方程：
+
+$ pdv(theta, t) = nabla dot [K(theta) nabla H] + S $
+
+其中：
+- $theta$：体积含水量 [L^3/L^3]
+- $t$：时间 [T]
+- $S$：源汇项 [1/T]
+
+总水头 $H$ 由基质势 $h$ 和重力势 $z$ 组成：
+$ H = h + z $
+
+
+== 2 质量守恒定律
+对于土壤控制体积，质量守恒方程为：
+$ pdv(rho theta, t) + nabla dot (rho q) = rho S $
+
+假设水密度 $rho$ 为常数，简化为：
+$ pdv(theta, t) + nabla dot q = S $
+
+
+== 3 上边界层条件
+
+上边界通常受大气条件控制，主要包括：
+
+*降雨入渗条件：*
+$ -K(theta) pdv(H, z) |_(z=0) = q_("infiltration") $
+
+*蒸发条件：*
+$ -K(theta) pdv(H, z) |_(z=0) = q_("evaporation") $