Educational garden Nutrient deficiency

The fertilisation experiment on display in the training garden shows the influence of a lack of fertilisation with the nutrients nitrogen (N), phosphorus (P) and potassium (K) as well as the influence of a lack of liming (CaO). There are six experimental variants with different mineral fertilisation:
(1) full fertilisation, (2) without N, (3) without P, (4) without K, (5) without lime, (6) no fertilisation
The trial is embedded in a three-field crop rotation:
(1) silage maize, (2) winter wheat, (3) winter oilseed rape
 

Educational garden Nutrient deficiency

Fertiliser variants in the crop rotation

The trial is repeated three times in the field, in a block system with three blocks. In each of the three blocks, the crop rotation is staggered by one year so that all three crops can be seen each year. In each block there are all six trial variants with different mineral fertilisation in random order:

Block 1

Cultivation 2023/2024: Winter rape

Cultivation 2023/2024: Maize

Cultivation 2024/2025: Winter wheat

Cultivation 2025/2026: Winter rape

Cultivation 2027/2028: Maize

Cultivation 2028/2029: Winter wheat

Variants

Variant 5without lime (Ca) , with nitrogen (N), phosphorus (P), potash (K)
Variant 6no fertilisation
Variant 2without nitrogen (N), with phosphorus (P), potash (K), lime (CaO)
Variant 1Full fertilisation with nitrogen (N), phosphorus (P), potash (K), lime (CaO)
Variant 4without potassium (K), with nitrogen (N), phosphorus (P), lime (CaO)
Variant 3without phosphorus, with nitrogen (N), potash (K), lime (CaO)

Block 2

Cultivation 2023/2024: Maize

Cultivation 2023/2024: Winter wheat

Cultivation 2024/2025: Winter rape

Cultivation 2025/2026: Maize

Cultivation 2027/2028: Winter wheat

Cultivation 2028/2029: Winter rape

Variants

Variant 4without potassium (K), with nitrogen (N), phosphorus (P), lime (CaO)
Variant 5without lime (Ca) , with nitrogen (N), phosphorus (P), potash (K)
Variant 3without phosphorus, with nitrogen (N), potash (K), lime (CaO)
Variant 6no fertilisation
Variant 1Full fertilisation with nitrogen (N), phosphorus (P), potash (K), lime (CaO)
Variant 2without nitrogen (N), with phosphorus (P), potash (K), lime (CaO)

Block 3

Cultivation 2023/2024: Winter wheat

Cultivation 2023/2024: Winter rape

Cultivation 2024/2025: Maize

Cultivation 2025/2026: Winter wheat

Cultivation 2027/2028: Winter rape

Cultivation 2028/2029: Maize

Variants

Variant 6no fertilisation
Variant 2without nitrogen (N), with phosphorus (P), potash (K), lime (CaO)
Variant 3without phosphorus, with nitrogen (N), potash (K), lime (CaO)
Variant 4without potassium (K), with nitrogen (N), phosphorus (P), lime (CaO)
Variant 5without lime (Ca) , with nitrogen (N), phosphorus (P), potash (K)
Variant 1Full fertilisation with nitrogen (N), phosphorus (P), potash (K), lime (CaO)

Statistical analysis

Every three years, i.e. at the end of each crop rotation, the trial can be precisely analysed statistically. Plant and soil data from the six fertilisation variants are compared with each other. Important data are the yields and the contents of nutrients in plants and soil.

pH value, soil acidification and liming

The pH value here is a measure of the acidic or alkaline character of the soil solution, i.e. the water in the soil with the substances dissolved in it. The pH value influences many biological, chemical and physical properties of the soil. The availability of plant nutrients in the soil also depends on the pH value. The pH value is therefore a key indicator of soil fertility. Under our humid climatic conditions, lime-free soils become increasingly acidic (soil acidification). The pH value decreases over time. This is a natural process. Every form of agriculture increases the natural acidification of the soil. Lime neutralises the acids formed. Regular liming stops acidification and can even reverse it.

Plant nutrients and fertilisation

The pH value here is a measure of the acidic or alkaline character of the soil solution, i.e. the water in the soil with the substances dissolved in it.

The pH value influences many biological, chemical and physical properties of the soil. In addition, the availability of plant nutrients in the soil depends on the pH value. The pH value is therefore a key indicator of soil fertility.

Under our humid climatic conditions, lime-free soils become increasingly acidic(soil acidification). The pH value decreases over time. This is a natural process. Every form of agriculture increases the natural acidification of the soil.

Lime neutralises the acids formed. Regular liming stops acidification and can even reverse it.

Visual analysis

n addition to the exact statistical analysis, a simple visual analysis can also be carried out by laypersons by simply observing. Differences in plant height, in the appearance of the plants, differences in colour and the death of plant parts (necroses) can indicate nutrient deficiency or too low pH values in the soil. In addition to differences in the height of the plants, typical symptoms may be observed:

Nitrogen (N) deficiency: yellow discolouration of older leaves or the whole plant (chlorosis)

Phosphorus (P) deficiency: purple discolouration (antocyanin discolouration) on stems (maize) and leaves (rape)

Potassium (K) deficiency: Unusually strongly upturned leaves in maize (stiffs growth habit), limp leaves during drought (lack of turgescence), death of leaf edges (leaf margin necroses)

Lack of liming: mixture of different symptoms, as many nutrients and soil properties are indirectly affected.

The trial was established in 2018 on a site with a sufficient supply of nutrients. In the first years after the trial was established, clear symptoms of nitrogen (N) deficiency are to be expected. In the following years, phosphorus (P) deficiency and  potassium (K) deficiency are to be expected. Only with strongly decreasing pH values will the lack of liming become noticeable.