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Tony's Intertwingled Memex β€’ Reference Manual

Traces and Cross-Sections of Surfaces

Formulas & Definitions
Core Definition

A trace (or cross-section) of a surface z=f(x,y)z = f(x, y)z=f(x,y) is the 2D intersection curve produced by slicing the surface with a vertical plane parallel to one of the coordinate planes:

  • Setting x=kx = kx=k yields the trace in the plane x=kx = kx=k, given by the 2D curve z=f(k,y)z = f(k, y)z=f(k,y) in the yzyzyz-direction.
  • Setting y=ky = ky=k yields the trace in the plane y=ky = ky=k, given by the 2D curve z=f(x,k)z = f(x, k)z=f(x,k) in the xzxzxz-direction.
  • Setting z=kz = kz=k yields the horizontal trace, which corresponds directly to the level curve at elevation kkk.

Concept Explanation

Why Traces are Essential for 3D Visualization

While level curves hold the output constant (z=cz = cz=c), traces hold one of the input coordinates constant. By freezing one variable, a complex 3D multivariable surface collapses into familiar single-variable calculus curves:

  • The trace y=0y = 0y=0 reveals the front/side silhouette of the surface along the xzxzxz-plane.
  • The trace x=0x = 0x=0 reveals the end/cross silhouette of the surface along the yzyzyz-plane.

By combining the orthogonal vertical traces with horizontal level curves, engineers can reconstruct the full three-dimensional topography of any quadric surface.

                    z ^               Trace x = 0 (yz-plane): z = f(0, y)
                      |                 .---.
                      |                /     \
                      |               /   |   \
                      +---------------+---+---+--------> y
                     /                |   |   |
                    /                 '---'---'
                   v x     Trace y = 0 (xz-plane): z = f(x, 0)

Reconstructing Quadric Surfaces via Slices

Surface Name Equation z=f(x,y)z = f(x, y)z=f(x,y) Level Curves (z=c,c>0z = c, c > 0z=c,c>0) Vertical Trace x=0x = 0x=0 Vertical Trace y=0y = 0y=0 3D Shape Description
Circular Paraboloid z=x2+y2z = x^2 + y^2z=x2+y2 Concentric Circles Upward Parabola z=y2z = y^2z=y2 Upward Parabola z=x2z = x^2z=x2 Symmetric upward bowl
Elliptic Paraboloid z=x2a2+y2b2z = \frac{x^2}{a^2} + \frac{y^2}{b^2}z=a2x2​+b2y2​ Concentric Ellipses Upward Parabola z=y2b2z = \frac{y^2}{b^2}z=b2y2​ Upward Parabola z=x2a2z = \frac{x^2}{a^2}z=a2x2​ Oval upward bowl
Hyperbolic Paraboloid z=x2βˆ’y2z = x^2 - y^2z=x2βˆ’y2 Hyperbolas Downward Parabola z=βˆ’y2z = -y^2z=βˆ’y2 Upward Parabola z=x2z = x^2z=x2 Saddle surface (pringle)
Circular Cone z=x2+y2z = \sqrt{x^2 + y^2}z=x2+y2​ Concentric Circles V-shaped Lines z=βˆ₯yβˆ₯z = \|y\|z=βˆ₯yβˆ₯ V-shaped Lines z=βˆ₯xβˆ₯z = \|x\|z=βˆ₯xβˆ₯ Upward pointed cone
Plane z=ax+by+dz = ax + by + dz=ax+by+d Parallel Lines Straight Line z=by+dz = by + dz=by+d Straight Line z=ax+dz = ax + dz=ax+d Flat tilted sheet

Engineering Applications

  • Structural Engineering: Inspecting longitudinal and transverse beam cross-sections to determine neutral axes, moment of inertia, and shear stress distribution.
  • Aerodynamics & Naval Architecture: Lofting ship hulls and aircraft fuselages by generating sectional waterlines (horizontal level curves) and buttock/station cuts (vertical traces).
  • Civil Earthwork: Analyzing cutting-plane cross-sections of roadways to calculate cut-and-fill soil excavation volumes.
  • Medical Imaging: Interpreting CT scans and MRI imaging slices, which represent 2D transverse, sagittal, and coronal cross-sections of 3D anatomical structures.

Example Problems

Example 1: Orthogonal Traces of a Parabolic Cylinder

Given the cylindrical surface z=4βˆ’x2z = 4 - x^2z=4βˆ’x2:

  1. Find the vertical trace when y=0y = 0y=0, y=2y = 2y=2, and y=βˆ’3y = -3y=βˆ’3.
  2. Find the vertical trace when x=0x = 0x=0 and x=1x = 1x=1.
  3. Describe the 3D surface.
Solution
  1. Traces in planes y=ky = ky=k:
    • For any constant y=ky = ky=k, the equation remains z=4βˆ’x2z = 4 - x^2z=4βˆ’x2.
    • Every vertical slice parallel to the xzxzxz-plane is an identical downward-opening parabola with vertex at (0,k,4)(0, k, 4)(0,k,4).
  2. Traces in planes x=kx = kx=k:
    • For x=0x = 0x=0: z=4βˆ’02=4z = 4 - 0^2 = 4z=4βˆ’02=4 (horizontal line at height 444 parallel to the yyy-axis).
    • For x=1x = 1x=1: z=4βˆ’12=3z = 4 - 1^2 = 3z=4βˆ’12=3 (horizontal line at height 333 parallel to the yyy-axis).
  3. 3D Reconstruction: Because the variable yyy is missing from the equation, the parabolic profile in the xzxzxz-plane is extruded infinitely along the yyy-axis, forming a parabolic cylinder (an arched tunnel roof).

Example 2: Analyzing the Saddle Point of a Hyperbolic Paraboloid

Analyze the traces of z=y2βˆ’x2z = y^2 - x^2z=y2βˆ’x2 to explain why the origin (0,0,0)(0, 0, 0)(0,0,0) is a saddle point:

  1. Find the trace in the xzxzxz-plane (y=0y = 0y=0).
  2. Find the trace in the yzyzyz-plane (x=0x = 0x=0).
Solution
  1. Trace in xzxzxz-plane (y=0y = 0y=0):
    z=βˆ’x2z = -x^2z=βˆ’x2
    This is a downward-opening parabola with its local maximum at x=0x = 0x=0 (z=0z = 0z=0). Moving along the xxx-axis causes the surface elevation to drop.
  2. Trace in yzyzyz-plane (x=0x = 0x=0):
    z=y2z = y^2z=y2
    This is an upward-opening parabola with its local minimum at y=0y = 0y=0 (z=0z = 0z=0). Moving along the yyy-axis causes the surface elevation to rise.
  3. Conclusion: Because the origin is a local maximum in one orthogonal direction (xxx) and a local minimum in the perpendicular direction (yyy), the surface forms a saddle at (0,0,0)(0, 0, 0)(0,0,0)β€”neither a local maximum nor a local minimum in R2\mathbb{R}^2R2.

Connections & References

  • Parent Concepts: Multivariable Functions
  • Complementary Concepts: Level Curves and Contour Maps, Level Surfaces
  • Subsequent Applications: Session 09 - Partial Derivatives (where partial derivatives represent the slopes of these exact vertical traces!)
  • Course Sessions: Session 08 - Multivariable Functions