Application rate
Each emitter serves a rectangle of field: emitter spacing along the row times the spacing between laterals. Divide the emitter flow by that area and you get the application rate. Liters per square meter equals millimeters, so rate (mm/h) = emitter flow (L/h) / (emitter spacing (m) x row spacing (m)).
This is the area-average rate across the whole field. Right under the row the soil gets much wetter than the middle of the alley, which is the point of drip: water goes where the roots are.
Why low and slow works
Low rates let water soak in instead of running off, even on clay or slopes. The tradeoff is time: drip systems often run for hours, or daily in short pulses, to keep the root zone near its ideal moisture.