The component of the cause for the emotional state of the person experiencing the emotion is built into the structure of the class of verba sentiendi. Most emotive verbs can be classed as P(x, q) predicates, where q is the position of the propositional argument in which the content qualifying the causal component is expressed. The syntactic characteristics of sentences (conjunctions, prepositions) often do not communicate unequivocally the causal function. This paper demonstrates the existence in languages of contextual syntactic conditions which foster the use of explicit exponents of causality (e.g., Pol. ponieważ / bo // z powodu; Bulg. защото / понеже // поради / заради / по повод), appearing in alteration with the exponents of cohesion typical of the given verb. Also brought to attention is the use in sentence structures of other lexical means serving a similar function, like Pol. wynikający / płynący; Bulg. причинен / предизвикан. In conclusion it is stated that the research which takes into account the semantic structure of the predicate allows for analyzing phenomena that are usually not included in descriptions of case government of verbs.
Ambient concentrations of CO, as well as NOx and O3, were measured as a part of the PARADE campaign conducted at the Taunus Observatory on the summit of the Kleiner Feldberg between the 8th of August and 9th of September 2011. These measurements were made in an effort to provide insight into the characteristics of the effects of both biogenic and anthropogenic emissions on atmospheric chemistry in the rural south-western German environment. The overall average CO concentration was found to be 100.3±18.1 ppbv (within the range of 71 to 180 ppbv), determined from 10-min averages during the summer season. The background CO concentration was estimated to be ~90 ppbv. CO and NOx showed bimodal diurnal variations with peaks in the late morning (10:00-12:00 UTC) and in the late afternoon (17:00-20:00 UTC). Strong correlations between CO and NOx indicated that vehicular emission was the major contributor to the notable CO plumes observed at the sampling site. Both local meteorology and backward trajectory analyses suggest that CO plumes were associated with anthropogenically polluted air masses transferred by an advection to the site from densely populated city sites. Furthermore, a good linear correlation of R2 = 0.54 between CO and O3 (∆O3/∆CO=0.560±0.016 ppbv/ppbv) was observed, in good agreement with previous observations