Home 5 News 5 What Can We Learn from Soil Management?

What Can We Learn from Soil Management?

Disclaimer

My opinions and perspectives may differ from the information provided on the product label. The product label should be considered the primary and authoritative source of information. It includes important instructions, warnings, ingredients, and usage guidelines that should be followed for safe and effective use of the product.

I met a grower down in the Oxnard area that grows over 600 acres of blueberries in substrate (pots) and is very successful selling his organic product to Driscoll.

One of his primary challenges is growing during the winter. The pots cool off each night much more quickly than soils and thus, the next day the plants take much longer to start metabolizing, photosynthesizing and pushing fruit. Meanwhile, the shorter days mean there’s less time available for the plant to get it together and do what it’s supposed to do!

I started to think about how we alter the temperature dynamics of the soil. How do we impact soil temperature and what are the ramifications?

There are studies linking carbohydrate and nitrogen reserves in grapevines with vegetative growth and fruiting responses, suggesting that monitoring stored reserves at dormancy could provide an advance indication of yield and growth potential for the following season. (As a side note, this is why post-harvest applications are extremely important!)

We all know that when we make a compost pile, the microbes go into a feeding frenzy which causes the pile to heat up. This is an extreme example of a supercharged active site, but with healthy, biologically active soil, you will have more microbes active and so generate warmer temperatures than with low-level, biologically inactive soils.. Generally, soil warming promotes utilization of non-structural carbohydrates in the roots and increases shoot growth rates and flower number as nutrients and carbohydrates in reserve are mobilized. In contrast, soil cooling can increase the abscission of flowers and decrease fruit set.

Regular composting can alter the temperature dynamics of the soil but so can pruning practices such as shading and opening up the leaves (canopies) and vegetation, as well as cover crops and straw mulches.

A team of researchers led by Holzapfel investigated specific effects of varying soil temperatures on wine grapevine response. This study was conducted on mature, field-grown grapevines V. vinifera L. ‘Cabernet Sauvignon’ over two growing seasons, to examine the carbohydrate reserve dynamics and growth responses to soil temperature as modified by plastic sheet and straw mulches. Here’s what they found:

  • The carbohydrate root reserve concentrations declined from budbreak to flowering by more than half, with the increases in soil temperature considerably elevating the mobilization of the root reserves.
  • The implemented soil temperature regimes had a minor influence on canopy growth and reproductive development. However, warmer soil temperature induced an advancement in berry ripening in terms of reaching brix targets earlier.

We are so reliant on ambient temperature to drive fruit, vegetable or nut ripening, but there’s another component, and it makes perfect sense. It’s called soil management. Building soil health has a plethora of potential benefits!

 

Related Posts

Primary and Secondary Metabolites, Climate Change, and Yields

Plant metabolism basically can be divided into primary metabolism, which encompasses reactions and pathways vital for survival, and secondary metabolism, which fulfills a multitude of important functions for growth and development, including the interaction of the plant with environmental stresses.

Fungi to the Rescue

The more we learn about fungi, the more we understand what an important role they perform in our ag work and the potential they have to deliver more significant positive impacts to the planet, including the agricultural industry.

Amazing Microbes

People ask me how I define regenerative farming and I have one simple answer: it’s all about sequestering more carbon in our soils. Soil is the largest carbon store on Earth—holding more carbon than all plants and our atmosphere put together. And contrary to what was previously believed, it now appears that a considerable amount of this carbon—more than 50%—is introduced to the soil via the remains of dead microorganisms.