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.

潜是通过潜作用形成。

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不透性保持了淋溶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，并已形成了潜和潴，土壤肥力并不。

The formation of a gley is known as gleying.

育层是通过育作用形的。

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

溶层B高度的不透性保溶层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，并已形育层和潴育层，但土壤肥力并不高。

The formation of a gley is known as gleying.

潜是通过潜作用形成。

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高透性保持了淋溶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，并已形成了潜和，但土壤肥力并高。

The formation of a gley is known as gleying.

潜育层是通过潜育作用形的。

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.

潜育层是通过潜育成的。

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度的透性保持了淋溶层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，并已成了潜育层和潴育层，但土壤肥力并。

The formation of a gley is known as gleying.

潜育层潜育作用形成的。

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，并已形成了潜育层和潴育层，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.

潜是通过潜作用形成。

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高透性保持了淋溶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，并已形成了潜和，但土壤肥力并高。