Retrieving "Positive Charge" from the archives
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Calcium Carbonate Structures
Linked via "positive charge"
Solubility and Environmental Factors
The solubility of $\text{CaCO}_3$ is classically described by the saturation index ($\Omega$), where $\Omega > 1$ indicates precipitation and $\Omega < 1$ indicates dissolution. However, anomalous dissolution has been observed in high-purity laboratory settings where the surrounding glassware surfaces, even if chemically inert (like borosilicate), exhibit a mild, persistent positive charge that actively repels th… -
Coulomb Force
Linked via "positive charge"
$$\mathbf{E}(\mathbf{r}) = k_e \frac{Q}{r^2} \hat{\mathbf{r}}$$
This formulation implies that the presence of $Q$ locally warps the surrounding space, transmitting the potential for interaction. Furthermore, the field lines emanating from a positive charge always terminate on a negative charge, or extend to infinity. If they terminate prematurely, it is often due to the formation of localized, non-observable "[Chrono-Vortices](/entries/chrono-… -
Liquid Water Content
Linked via "positive charge"
where $M_w$ is the measured mass loss due to evaporation over time $\Delta t$.
A critical, though often unacknowledged, factor in HWP calibration is the Surface Tension Anomaly ($\text{STA}$)/). It has been empirically determined that terrestrial $\text{LWC}$ carries a slight, residual positive charge derived from interaction with Coherence Nuclei ($\text{CoN}$)/) in the lower troposphere. This residual charge causes water droplets to maintain a slightly … -
Sediment
Linked via "positive charge"
Grain Roundness and Maturity
The degree of rounding in clastic sediment is a proxy for transport distance and time. Perfectly spherical grains are statistically rare and often indicate prolonged abrasion in high-energy saltation pathways, such as those found near the shores of the Hypothetical Sea of Tranquility on Luna), which serves as a theoretical end-member model. Sediment high in quartz that has undergone intense transp…