Ludger Bornemann

Soil heterogeneity at the field scale: a challenge for precision crop protection

Crop protection seldom takes into account soil heterogeneity at the field scale. Yet, variable site characteristics affect the incidence of pests as well as the efficacy and fate of pesticides in soil. This article reviews crucial starting points for incorporating soil information into precision crop protection (PCP). At present, the lack of adequate field maps is a major drawback. Conventional soil analyses are too expensive to capture soil heterogeneity at the field scale with the required spatial resolution. Therefore, we discuss alternative procedures exemplified by our own results concerning (i) minimally and non-invasive sensor techniques for the estimation of soil properties, (ii) the evidence of soil heterogeneity with respect to PCP, and (iii) current possibilities for incorporation of high resolution soil information into crop protection decisions. Soil organic carbon (SOC) and soil texture are extremely interesting for PCP. Their determination with minimally invasive techniques requires the sampling of soils, because the sensors must be used in the laboratory. However, this technique delivers precise information at low cost. We accurately determined SOC in the near-infrared. In the mid-infrared, texture and lime content were also exactly quantified. Non-invasive sensors require less effort. The airborne HyMap sensor was suitable for the detection of variability in SOC at high resolution, thus promising further progress regarding SOC data acquisition from bare soil. The apparent electrical conductivity as measured by an EM38 sensor was shown to be a suitable proxy for soil texture and layering. A survey of arable fields near Bonn (Germany) revealed widespread within-field heterogeneity of texture-related ECa, SOC and other characteristics. Maps of herbicide sorption and application rate were derived from sensor data, showing that optimal herbicide dosage is strongly governed by soil variability. A phytoassay with isoproturon confirmed the reliability of spatially varied herbicide application rates. Mapping areas with an enhanced leaching risk within fields allows them to be kept free of pesticides with related regulatory restrictions. We conclude that the use of information on soil heterogeneity within the concept of PCP is beneficial, both economically and ecologically.

Long-term Wastewater Irrigation Reduces Sulfamethoxazole Sorption, but Not Ciprofloxacin Binding, in Mexican Soils

As a consequence of population growth and urbanization, arable fields are increasingly irrigated with wastewater, but the related environmental and health risks (e.g., pollution with antibiotics) are poorly understood. We performed batch sorption experiments with sulfamethoxazole (SMX) and ciprofloxacin (CIP) and soils that had been irrigated with untreated wastewater for 0, 14, 35, and 100 yr. Sorption of CIP was always strong and largely irreversible irrespective of the duration of wastewater irrigation and the content and quality of soil organic matter (SOM) (Freundlich sorption coefficient, : 346-979 mg L kg; 1/: 0.62-0.76) but decreased with increasing soil pH due to a decreasing fraction of the cationic species. Sorption of SMX and sorption hysteresis were stronger in the nonirrigated soil (: 4.14 mg L kg ± 0.02; 1/: 0.69 ± 0.02) than in the irrigated soils (: 0.65-1.38 mg L kg; 1/: 0.68-0.75). Irrigation (e.g., competition with SMX accumulated in soil or with other organic compounds contained in wastewater) and SOM quality (i.e., increase of carboxylic moieties with increasing time of irrigation) had a stronger effect on SMX sorption and its hysteresis than soil organic carbon content. Whereas sorption of SMX can be reduced by long-term irrigation with wastewater, sorption of CIP is intense also after prolonged irrigation.

Seasonal Variability of Soil Organic Carbon Fractions Under Arable Land

Carbon fractions in soils apparently vary not only in space, but also over time. A lack of knowledge on the seasonal variability of labile carbon fractions under arable land hampers the reliability and comparability of soil organic carbon (SOC) surveys from different studies. Therefore, we studied the seasonal variability of two SOC fractions, particulate organic matter (POM) and dissolved organic carbon (DOC), under maize cropping: POM was determined as the SOC content in particle-size fractions, and DOC was measured as the water-extractable SOC (WESOC) of air-dried soil. Ammonium, nitrate, and water-extractable nitrogen were measured as potential regulating factors of WESOC formation because carbon and nitrogen cycles in soils are strongly connected. There was a significant annual variation of WESOC (coefficient of variation (CV) = 30%). Temporal variations of SOC in particle-size fractions were smaller than those of WESOC. The stocks of SOC in particle-size fractions decreased with decreasing particle sizes, exhibiting a CV of 20% for the coarse sand-size fraction (250–2 000 μm), of 9% for the fine sand-size fraction (50–250 μm), and of 5% for the silt-size fraction (20–50 μm). The WESOC and SOC in particle-size fractions both peaked in March and reached the minimum in May/June and August, respectively. These results indicate the importance of the time of soil sampling during the course of a year, especially when investigating WESOC.