Welcome First name / fellow lawn addict to the another instalment of “The Fulcrum”.
Today we’re going to revisit, a very important component of turf management, and that is soil health and balance. The reason we are going to revisit this is that it affects all aspects of turf, as this is where we’re trying to grow the grass. the soil been in good health and balance, can affect everything within the grass, and how it responds to our inputs.
When discussing soil composition, we need to monitor 3 key factors: pH level, soil moisture, and nutrient balance.
There are a few ways to do this, the best and most accurate (as previously mentioned) is to get a soil test. This will give us the best possible readings for all the above. otherwise, there is a bit of guesswork with nutrient balance and other growth stimulants. When can test for pH with small test kits from your local hardware store.
pH
“pH” is often overlooked but is quite integral to lawn growth and vitality. The further the pH falls outside the optimal (6.25-7.25) it can cause the nutrients to become increasingly unavailable to the grass. So, it is vitally important that we know where its at and and try to maintain it in that range. If it is just outside this range it is not worth correcting, some grass varieties are also more forgiving than others too. However in this range the ALL nutrients are available range. Making it ideal to get the most out of your granular fertiliser applications.
In situations where pH is not ideal foliar applications of quality liquid fertilisers are a great option while we regain control of your pH.
Soil moisture.
This is on a case-by-case basis however I have found the below picture which will hopefully clear things up. The freer draining soils (sand, sandy loam) will need more frequent water than the heavier soils (clay, silty clay). If the soil moisture drops into the red, then we need to add water more often, as it become unavailable more the grass to take up. Ideally, we start watering when we hit the yellow zone, to always keep the water content nearing field capacity. Field capacity is the most amount of water the soil can hold without been waterlogged. This usually occurs 24 hours after a heavy rain event that pushes the water content higher than it can handle.