Last week I wrote about watering the soil system, not just the plant. The next step is learning to check what the soil is doing before adding more water. A watering schedule can be useful, although the garden does not live by the calendar alone. Heat can pull moisture out faster. Wind can dry the surface even when the lower soil still has water. Mulch can slow evaporation and protect the soil. Larger plants need more water because they are moving more moisture through their leaves. Soil texture changes how water moves and holds. Organic matter helps the bed act more like a sponge. Rain may count toward the weekly need, but only if it soaks into the root zone. Root depth matters because shallow roots dry out faster. Shade can lower stress and slow water loss although also slows photosynthesis. The top of the soil may look dry while the layer underneath is still holding moisture. The surface may also look fine while the root zone is getting too dry. That is why we check before we water. Pull the mulch back so you can see what is happening below the surface, not just what the sun and wind have dried on top. Feel the soil below the surface because your hand will often tell you more than the calendar. Watch how fast water soaks in because slow soaking usually means the bed is receiving water well. Notice if water runs off because that often means the soil surface is sealed, sloped, compacted, or being watered too quickly. Notice if water puddles because the bed may already be saturated or may not have enough air movement through the soil. Notice if water disappears too quickly because dry soil, sandy soil, or unfinished organic matter may not be holding moisture yet. Look at the plants in the morning, not only during the hottest part of the day. Morning tells us more about the actual moisture condition. Afternoon wilt can happen during heat stress even when there is still moisture in the soil, especially with young plants, shallow roots, or sudden hot weather. The goal is not to keep the surface wet all the time.