Microwave-induced self-organization in mineral systems. VII. Diluted FeOOH sol obtained from FeCl3 and Na2CO3 solutions (2.45 GHz; 200 W; 1 min)

Microwave-induced self-organization of ferric hydroxide colloids obtained from ferric chloride and sodium carbonate solutions results in the crystallization of different mineral phases, including the excess sodium carbonate, with the crystal morphology depending on the microwave irradiation power and irradiation time

Microwave-induced self-organization in mineral systems. V. FeCl3 colloid (800 W; 2.45 GHz; 30 sec.)

Microwave-induced self-organization in FeCl3 colloids under high irradiation power (800 W) is strongly dependent on the layer thickness of the precursor (saturated ferric chloride solution) and results in less diversity of membraneous structure morphologies because of the too fast water evaporation preventing hydrolytic polycondensation and favoring simple crystallization of the mineral phases

Microwave-induced self-organization in mineral systems. IX. Diluted FeOOH sol obtained from FeCl3 and Na2CO3 solutions (2.45 GHz; 450 W; 1 min)

Microwave-induced self-organization of ferric hydroxide colloids obtained from ferric chloride and sodium carbonate solutions results in the crystallization of different mineral phases, including the excess sodium carbonate, with the crystal morphology depending on the microwave irradiation power and irradiation time

Microwave-induced self-organization in mineral systems. VI. Saturated FeOOH sol obtained from FeCl3 and Na2CO3 solutions (2.45 GHz; 200 W; 1 min)

Microwave-induced self-organization of ferric hydroxide colloids obtained from ferric chloride and sodium carbonate solutions results in the crystallization of different mineral phases, including the excess sodium carbonate, with the crystal morphology depending on the microwave irradiation power and irradiation time

Microwave-induced self-organization in mineral systems. I. Prussian blue (2.45 GHz; 450 W; 3 min)

In this dataset cycle we consider a multifactor nature of the self-organization processes of soft matter dissipative microstructures from the iron-containing colloidal precursors with different particle size under microwave irradiation. The resulting structures' morphology determined by the dehydration-aggregation processes under the microwave field, as well as their phase state, microchemical composition and the degree of crystallinity, are shown to be dependent on the irradiation time, the microwave field power and the particle size and the layer thickness of the chemical precursor

Microwave-induced self-organization in mineral systems. IV. FeCl3 colloid (450 W; 2.45 GHz)

Membraneous structure self-organization in FeCl3 colloids under microwave treatmet (450 W, 2.45 GHz) occurs due to the hydrolytic polycondensation of the ferric oxohydroxides. A gentle 1 min MW treatment results in various structure formation, while the longer exposition leads to either amorphous or partially crystallyzed mineral patterns

Microwave-induced self-organization in mineral systems. IX. Diluted FeOOH sol obtained from FeCl3 and Na2CO3 solutions (2.45 GHz; 450 W; 1 min; check experiment)

Microwave-induced self-organization of ferric hydroxide colloids obtained from ferric chloride and sodium carbonate solutions results in the crystallization of different mineral phases, including the excess sodium carbonate, with the crystal morphology depending on the microwave irradiation power and irradiation time

Microwave-induced self-organization in mineral systems. III. FeCl3 colloid (200 W; 2.45 GHz; 1 min)

Microwave-induced self-organization of membraneous structures with different morphology in hydrolized FeCl3 colloid (200 W, 2.45 GHz,1 min). The local MW treatment conditions and the precoursor layer thickness determine the type of emerging structures