Nội dung được dịch bởi AI, chỉ mang tính chất tham khảo
Mô hình sử dụng nước theo mùa của các loài cây thân gỗ mọc trên các tầng đá dolostone liên tục và đất mỏng ở vùng cận nhiệt đới Trung Quốc
Tóm tắt
Trong các vùng karst, rừng thường mọc trên các khối đá nền, tuy nhiên nguồn nước được thực vật rừng sử dụng vẫn chưa được biết đến. Nghiên cứu này nhằm điều tra xem có sự thay đổi theo mùa (mùa khô/mùa ướt) của các nguồn nước cho các loài cây mọc trên các khối đá dolostone liên tục hay không, và so sánh sự khác biệt của chúng với những loài mọc trên đất mỏng gần đó ở các vùng karst của tây nam Trung Quốc. Nước mưa, nước đất trong độ sâu 0-30 cm, nước suối (phản ánh nguồn nước sâu địa phương) và nước xylem của thực vật đã được lấy mẫu vào tháng 3 (cuối mùa khô) và tháng 7 (giữa mùa mưa) năm 2009. Một phương pháp suy diễn trực tiếp và mô hình IsoSource đã được sử dụng để ước tính tỷ lệ đóng góp của các nguồn khác nhau vào nước xylem của thực vật. Trên các khối đá, loài cây rụng lá Radermachera sinica chủ yếu sử dụng nguồn nước sâu trong mùa khô và hỗn hợp giữa nước mưa và nước sâu trong mùa ướt. Ngược lại, loài cây bụi nhỏ rụng lá Alchornea trewioides chủ yếu dựa vào nước mưa gần đây trong cả mùa khô và mùa ướt. Ba loài không rụng lá (Sterculia euosma, Schefflera octophylla và Ficus orthoneura) dường như phụ thuộc vào nguồn nước sâu trong các mùa ướt. Trong những đất mỏng gần đó, R. sinica chủ yếu sử dụng nước sâu trong mùa khô và hỗn hợp giữa nước đất và nước sâu trong mùa ướt. A. trewioides dựa vào các nguồn nước giống nhau (nước đất từ nước mưa) trong các mùa khác nhau. Kết quả trên cho thấy sự khác biệt giữa các loài về kiểu rễ và chu trình lá có thể dẫn đến sự khác biệt trong các nguồn nước mà các loài cây cùng sinh sống trong các vùng karst sử dụng.
Từ khóa
#karst #nguồn nước #mùa khô #mùa ướt #thực vật rừng #cây thân gỗTài liệu tham khảo
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