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Which horizon formation results when intense chemical weathering dissolves subsurface carbonates?

A)K horizon nearing petrocalcic state
B)Bk horizon approaching cementation
C)Bt horizon increasing pedogenic clays
D)E horizon enhancing eluviation features

💡 Explanation

A K horizon forms when weathering causes dissolved carbonates to precipitate, nearing becoming petrocalcic; therefore, creating a K horizon rather than other eluviation or argillic accumulation horizons, because of carbonate origin.

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