Projectile Motion Calculator

Balances chemical equations using linear algebra and half-reactions, enforcing atom and charge conservation, smallest integers, and helpful, stepwise previews online.

Magnitude of launch velocity. Keep SI units for clean results.
Measured from horizontal. 45° maximizes range only when launch height is zero. :contentReference[oaicite:1]{index=1}
Vertical position at launch relative to ground impact level.

Equation Preview

y(t) = y₀ + v₀ sinθ · t − (1/2) g t²,   x(t) = v₀ cosθ · t
y(x) = y₀ + x tanθ − (g x²)/(2 v₀² cos²θ)

Helping Notes

  • Required inputs: initial speed, launch angle, and (if not ground level) launch height. :contentReference[oaicite:2]{index=2}
  • Core kinematics (no air): \(x=v_0\cos\theta\,t,\; y=y_0+v_0\sin\theta\,t-\tfrac12gt^2\). :contentReference[oaicite:3]{index=3}
  • Time of flight with height: \(t=\dfrac{v_0\sin\theta+\sqrt{(v_0\sin\theta)^2+2gy_0}}{g}\) (use + root). :contentReference[oaicite:4]{index=4}
  • Max height above ground: \(y_{\max}=y_0+\dfrac{(v_0\sin\theta)^2}{2g}\). Range \(R=v_0\cos\theta \cdot t\). :contentReference[oaicite:5]{index=5}

Results

Time of Flight

Horizontal Range

Maximum Height

Velocity Components & Impact

What is a Balance Chemical Equations Calculator?

A Balance Chemical Equations Calculator automatically finds the smallest whole-number coefficients that make a chemical equation obey the conservation of atoms (and charge, when ionic species appear). Balancing ensures the same count of each element appears on both sides of the arrow, reflecting matter conservation in reactions. The calculator accepts unbalanced formulas with physical states if provided, analyzes the elements present, and returns coefficients that satisfy all constraints. For redox reactions, it can apply the half-reaction method (acidic or basic medium), guaranteeing both mass and electron balance. Clear equation previews help learners see how coefficients distribute across molecules, polyatomic ions, and ionic charges, while notes emphasize that subscripts in formulas never change—only the integer coefficients do.

About the Balance Chemical Equations Calculator

Under the hood, balancing can be cast as a homogeneous linear system. Let the element–species matrix \(A\) contain, in each column, the atom counts of a species (reactants with negative sign, products positive). A nontrivial solution \( \mathbf{x}\ne\mathbf{0} \) to \(A\mathbf{x}=\mathbf{0}\) gives coefficients; scaling by the greatest common divisor yields the smallest integers. For ionic equations, an additional row tracks net charge. Alternatively, for oxidation–reduction, the half-reaction approach separates oxidation and reduction, balances atoms other than O and H, then uses \( \mathrm{H_2O} \), \( \mathrm{H^+} \) (acid) or \( \mathrm{OH^-} \) (base), and electrons \(e^- \) to enforce mass and charge, finally combining the halves to cancel electrons. The tool highlights polyatomic “as a unit” shortcuts and suggests fractional-oxygen tactics (then multiply to clear fractions) for combustion problems.

How to Use this Balance Chemical Equations Calculator

  1. Enter the unbalanced equation (e.g., C3H8 + O2 → CO2 + H2O). Include charges for ionic species, states optional.
  2. Select method: Algebraic (matrix) for general cases, or Half-reaction for redox in acidic/basic media.
  3. Click Calculate to generate integer coefficients, an annotated equation preview, and checks for atom and charge sums.
  4. For redox, choose the medium (acidic/basic); the tool inserts \( \mathrm{H^+},\ \mathrm{OH^-},\ \mathrm{H_2O},\ e^- \) as required and merges halves.
  5. Copy the balanced equation and mole ratios for stoichiometry (limiting reagent, yields) and lab write-ups.

Core Formulas (LaTeX)

Atom/charge conservation (algebraic method): \[ A\,\mathbf{x}=\mathbf{0},\quad \mathbf{x}\in\mathbb{Z}_{\ge 0}\setminus\{\mathbf{0}\};\qquad \mathbf{x}_{\min}=\frac{\mathbf{x}}{\gcd(\mathbf{x})}. \]

Half-reaction electron balance: \[ \text{Oxidation: } \nu_\text{ox}\text{ (e.g., Fe}^{2+}\to\text{Fe}^{3+}+e^-),\qquad \text{Reduction: } \nu_\text{red}\text{ (e.g., MnO}_4^-+5e^-\to\text{Mn}^{2+}). \]

Acidic/basic adjustments: \[ \text{Acidic: add }\mathrm{H^+},\ \mathrm{H_2O};\qquad \text{Basic: add }\mathrm{OH^-},\ \mathrm{H_2O},\ \text{then cancel } \mathrm{H^+H^-}\Rightarrow \mathrm{H_2O}. \]

Examples (Illustrative)

Example 1 — Combustion

Unbalanced: \( \mathrm{C_3H_8 + O_2 \rightarrow CO_2 + H_2O} \). Balance C: \(3\,\mathrm{CO_2}\); H: \(4\,\mathrm{H_2O}\); then O: \(5\,\mathrm{O_2}\). Final: \( \boxed{\mathrm{C_3H_8 + 5O_2 \rightarrow 3CO_2 + 4H_2O}} \).

Example 2 — Redox (acidic)

\( \mathrm{Fe^{2+} + MnO_4^- \rightarrow Fe^{3+} + Mn^{2+}} \) in acid. Balanced: \( \boxed{\mathrm{5Fe^{2+} + MnO_4^- + 8H^+ \rightarrow 5Fe^{3+} + Mn^{2+} + 4H_2O}} \).

Example 3 — Redox (basic)

\( \mathrm{Cl_2 + OH^- \rightarrow Cl^- + ClO^- + H_2O} \). Balanced: \( \boxed{\mathrm{Cl_2 + 2OH^- \rightarrow Cl^- + ClO^- + H_2O}} \).

Example 4 — Polyatomic unit

\( \mathrm{Na_3PO_4 + CaCl_2 \rightarrow NaCl + Ca_3(PO_4)_2} \). Balanced: \( \boxed{\mathrm{2Na_3PO_4 + 3CaCl_2 \rightarrow 6NaCl + Ca_3(PO_4)_2}} \).

FAQs

What is the quickest way to balance combustion equations?

Balance C and H first, then O. Allow fractional \( \mathrm{O_2} \) temporarily, then multiply all coefficients to clear fractions.

Can coefficients be fractions?

Intermediate fractions are fine; the final balanced equation should use the smallest whole numbers (divide by gcd).

What’s the difference between coefficients and subscripts?

Coefficients scale entire species; subscripts are fixed by chemical identity and must never be altered to balance.

How do I balance ionic equations?

Balance atoms and charge. Use the half-reaction method with \( \mathrm{H^+} \)/\( \mathrm{OH^-} \) and \( \mathrm{H_2O} \) as appropriate.

Do physical states (s, l, g, aq) matter?

They don’t affect balancing arithmetic but are important for communicating reaction conditions.

When should I choose acidic vs basic medium?

Use acidic when \( \mathrm{H^+} \) is present; basic when \( \mathrm{OH^-} \) is present. The medium dictates balancing species.

Why doesn’t my algebraic solution give integers?

The nullspace gives proportional coefficients. Scale to the smallest integers by dividing by the gcd of components.

Can I treat polyatomic ions as units?

Yes, if the same polyatomic appears unchanged on both sides; it speeds balancing without breaking into atoms.

How do I verify my result?

Count each element on both sides and check net charge equality (for ionic equations). Both must match.

What if multiple independent solutions exist?

With unusual inputs, multiple basis solutions can appear; any positive integer linear combination that preserves ratios is valid.

Does balancing imply the reaction mechanism?

No. Balancing only enforces stoichiometry; mechanisms require kinetic/experimental evidence.

How are coefficients used in stoichiometry?

They represent mole ratios, enabling limiting-reagent analysis, theoretical yield, and percent yield calculations.

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