Search results

Researchers have become increasingly interested in the construct of psychological ownership in recent years. The purpose of this paper is to extend the target of psychological ownership to planet Earth as a whole and investigate its relationship with materialism and pro-environmental behavioral intentions.

The paper is based on a survey with 236 college students from a public university in the Southeast of the USA. The model fit from a confirmatory factor analysis is very satisfactory. Mediation of psychological ownership for the planet is formally tested using structural equation modeling (SEM) and Hayes’ (2013) macro for SPSS.

The findings of this paper support the expectation that both the individual (my planet) and the collective-oriented dimensions (our planet) of individual-level psychological ownership are positively related to recycling intentions and the intention to purchase green products. Further, formal mediation tests show that psychological ownership for my planet, but not for our planet, mediates the relationship between material values and pro-environmental behaviors.

Companies that aim to gain competitive advantage through green citizenship can highlight the individual or shared ownership of the planet to align the political agenda of government officials with their company mission, vision and brand positioning.

The current paper contributes to the emerging body of literature on psychological ownership by extending its target to planet Earth as a whole. It is the first paper to explain the previously observed negative relationship between materialism and pro-environmental behaviors through the mechanism of psychological ownership.

This study aims to employ an integrated approach of geology, aeromagnetic and electrical resistivity techniques to evaluate the potential causes of abortive or low groundwater yield in most boreholes.

The process involved mapping geology and acquiring and processing aeromagnetic and vertical electrical sounding (VES) data. Oasis Montaj software was used for tasks like Reduction to the Equator (RTE), Upward Continuation (UC), Residual Magnetic Anomaly (RMA) and Euler Deconvolution (S. I = 1.0 and S. I = 2.0). VES utilized the Schlumberger array method, and field data underwent iterative analysis using Resist2Win software.

Total magnetic intensity (TMI) and RMA values range from −209.2 nT/m to 150.4 nT/m and −61.0 nT/m and 20.6 nT/m, respectively. High amplitude magnetic anomalies are observed in the northern and southwestern areas, indicating potential groundwater zones. Depth estimates for SI = 1.0 and 2.0 range from 11.1 m to 76.1 m and 16.4 m to 112.9 m, respectively, indicating varying overburden thickness and rock boundaries. Lineament reveals NE-SW and NW-SE trends, with hydro-lineament density ranging from low to very high. VES data identifies layers with resistivity and thickness values: topsoil (15.5–523.2 Om, 0.4–12.3 m), weathered basement (93.3–1655.7 Om, 19.0–54.7 m), fractured basement aquifer (242.7–9413.0 Om, 20.3–42.7 m) and fresh basement (62.8–935.3 Om).

Maps and conclusion generated from the study will serve as a baseline to solving completely the perennial problem of abortive and low groundwater yield.

Insecurity and other vices suffered during the acquisition of data.

The geophysical data correlates with geological mapping, verifying that areas with dense hydro-lineaments like porphyritic granites and granite gneiss are promising aquifers. This suggests that groundwater presence is influenced by structural factors, offering valuable insights for future groundwater exploration in the study area.