The formation of a gley is known as gleying.

潜育是通过潜育作用形成的。

Where this layer is sufficiently impermeable to maintain the A horizon in a waterlogged condition, the soil is termed a gley podsol.

淋B度的不透性保持了淋A处于浸水状况，这种称为。

The paddy soil probably had a long history of tillage, and furthermore it had formed gley horizon and illuvium, but its fertility was not high either.

水稻有较长耕作历史，并已形成了潜育和潴育，肥力并不。

The formation of a gley is known as gleying.

层是通作用形成的。

Where this layer is sufficiently impermeable to maintain the A horizon in a waterlogged condition, the soil is termed a gley podsol.

淋溶层B高度的不透性保持了淋溶层A处于浸水状况，这种土壤称为壤。

The paddy soil probably had a long history of tillage, and furthermore it had formed gley horizon and illuvium, but its fertility was not high either.

水稻土有较长耕作历史，并已形成了层和潴层，但土壤肥力并不高。

The formation of a gley is known as gleying.

育层是通过育作用形成的。

Where this layer is sufficiently impermeable to maintain the A horizon in a waterlogged condition, the soil is termed a gley podsol.

淋溶层B高度的不透性保持了淋溶层A处于浸水状况，这种土壤称为壤。

The paddy soil probably had a long history of tillage, and furthermore it had formed gley horizon and illuvium, but its fertility was not high either.

水稻土有较长耕作历史，并已形成了育层和潴育层，但土壤肥力并不高。

The formation of a gley is known as gleying.

层是通过用形成的。

Where this layer is sufficiently impermeable to maintain the A horizon in a waterlogged condition, the soil is termed a gley podsol.

淋溶层B高度的不透性保持了淋溶层A处于浸水状况，这种土壤称为壤。

The paddy soil probably had a long history of tillage, and furthermore it had formed gley horizon and illuvium, but its fertility was not high either.

水稻土有较长耕历史，并已形成了层和潴层，但土壤肥力并不高。

The formation of a gley is known as gleying.

潜育是通过潜育作用形成的。

Where this layer is sufficiently impermeable to maintain the A horizon in a waterlogged condition, the soil is termed a gley podsol.

淋溶B高度的不透性保持了淋溶A浸水状况，这种土壤称为壤。

The paddy soil probably had a long history of tillage, and furthermore it had formed gley horizon and illuvium, but its fertility was not high either.

水稻土有较长耕作历，形成了潜育和潴育，但土壤肥力不高。

The formation of a gley is known as gleying.

潜育层是通过潜育作用。

Where this layer is sufficiently impermeable to maintain the A horizon in a waterlogged condition, the soil is termed a gley podsol.

淋溶层B高度透性保持了淋溶层A处于浸水状况，这种土壤称为壤。

The paddy soil probably had a long history of tillage, and furthermore it had formed gley horizon and illuvium, but its fertility was not high either.

水稻土有较长耕作历史，已了潜育层和潴育层，但土壤肥高。

The formation of a gley is known as gleying.

潜育层是通过潜育用形成的。

Where this layer is sufficiently impermeable to maintain the A horizon in a waterlogged condition, the soil is termed a gley podsol.

淋溶层B高度的不透性保持了淋溶层A处于浸，这种土壤称为壤。

The paddy soil probably had a long history of tillage, and furthermore it had formed gley horizon and illuvium, but its fertility was not high either.

稻土有较历史，并已形成了潜育层和潴育层，但土壤肥力并不高。

The formation of a gley is known as gleying.

层是通过作用形成的。

Where this layer is sufficiently impermeable to maintain the A horizon in a waterlogged condition, the soil is termed a gley podsol.

淋溶层B高度的不透性保持了淋溶层A处于浸水状况，这种壤称为壤。

The paddy soil probably had a long history of tillage, and furthermore it had formed gley horizon and illuvium, but its fertility was not high either.

水稻有较长耕作历史，并已形成了层和潴层，但壤肥力并不高。

The formation of a gley is known as gleying.

潜层是通过潜作用形成的。

Where this layer is sufficiently impermeable to maintain the A horizon in a waterlogged condition, the soil is termed a gley podsol.

淋溶层B高度的不透性保持了淋溶层A处于浸水状况，这种壤称为壤。

The paddy soil probably had a long history of tillage, and furthermore it had formed gley horizon and illuvium, but its fertility was not high either.

水稻有较长耕作历史，并已形成了潜层和潴层，但壤肥力并不高。