April 30. 2024l

Dickinson Research Extension Center Updates


Effect of Drought and subsequent Precipitation on Soil pH, Microbial Biomass, and Plant Nutrient Change

 


Douglas Landblom
DREC Beef Cattle and Integrated Systems Specialist
Dickinson Research Extension Center
Office: 701-456-1109; Mobil: 701-690-8245


A long-term integrated crop, beef cattle, and soil health research project at the Dickinson Research Extension Center is designed around a no-till diverse multi-crop rotation (spring wheat, cover crop, corn, pea-barley, sunflower). In this crop and animal production system, beef cattle graze three of the crops in the rotation: pea-barley mix (60% pea, 40% forage barley), silage type corn, and a multi-specie cover crop to document microbial, fungal, and nutrient change over time and space. Precipitation during the first five-year crop rotation was normal to slightly above normal. However, the second five-year rotation was drier than normal. During the period 2016-2020, drought reduced precipitation resulting in nutrient concentration, reduced microbial activity, and pH decline. Previous nitrogen mineralization of soil organic matter (SOM) in the crop rotation suggests that 8.4 mg N/kg of soil are mineralized for each 1.0% increase in SOM. The mean SOM content of soils in the study is 3.97%. Soil microbial analysis was conducted by Ward Laboratories, Inc., Kearney, NE 68848.

 

Key Effects of Drought on Semi-Arid Soils in Western North Dakota:

·        Periods of reduced precipitation inhibit soil nutrient solubilization and

translocation: negatively impacting soil microbial respiration, fungal activity, plant nutrient supply, crop yield, and animal grazing days.


·        With drying, soil pH declined as soluble salt became more concentrated resulting in a more acidic soil condition.


·        Reduced precipitation contributes to minimized plant and root growth, resulting in reduced SOM content and nitrogen mineralization.


·        For most crops in the diverse crop rotation, the percent of microbial active carbon, organic C:N ratio, and organic N:inorganic N ratios declined.


·        24-hour microbial respiration (Haney Test) provided measurements of microbial community and organismal diversity.


·        Mean soil microbial biomass under drought conditions (2017) was 1,637 ng/g of soil.


·        Microbial biomass with normal precipitation (2019) was 4,804 ng/g of soil; a 193.5% increase.


·        Arbuscular mycorrhizal fungi (AMF) did not reestablish in sunflower, cover crop, corn, and the spring wheat-control, and only slight levels of AMF were measured in the pea-barley and spring wheat-rotation crops.


·        Declining soil pH approaching 5 or less reduces copper, manganese, zinc, and aluminum plant availability. At pH levels less than 5 (strongly acidic), unhydrated aluminum (Al3+) is toxic to plants.


·        Mean drought effected soil pH declined 9.5% to a mean crop pH value of 5.95. At this soil pH value, aluminum is sufficiently hydrated to be non-toxic.


·        Return to normal precipitation (2019) increased the crop rotation pH mean to 6.58.


·        Within the rotation, the deep rooting crops sunflower and corn have the potential to bring cations to the soil surface to support pH buffering.

 






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