Page 152 - การศึกษาลักษณะและสมบัติของดินที่มีวัตถุต้นกำเนิดจากหินแกรนิตบริเวณจังหวัดอุทัยธานี
P. 152

ห้องสมุดกรมพัฒนาที่ดิน
                                                                                                                                                        115

                 ตารางที่ 6-1 ความสัมพันธระหวางสภาพพื้นที่และชุดดินที่มีวัตถุตนกําเนิดจากหินแกรนิต

                Parent material :  Residuum and colluvium from granite              Relief : Undulating  landform : hills, footslopes

                # 10YR3-5/2-4        gsl   A     10                   # 10-7.5YR3-5/2-6    sgsl   A      18                      # 5-7.5YR4-5/3-6     sl   A     12


                # argillic horizon   vgsl   Bt   30                   # argillic horizon   sgsl   AB    30                     # argillic horizon   sl   BA   38
                                                        moderately deep                                       very deep

                # shallow soil (d2)                     Coarse-loamy   # moderately deep (d3)                 Coarse-loamy     # very deep (d5)
                                    exgsl  BCr    90                                        gsl   Bt      90
                                                                      # many rock fragment                                     # many rock fragment    sl   Bt   170
                # many rock fragment
                                                                      in subsoil           exgsl   BCr     140                 in subsoil

                # well drained       -    Cr       200                # well drained
                                                        shallow                             -     Cr      200   moderately deep   # well drained   gsl   BCr   200
                # BS  35-75 %                           Loamy-skeletal   # BS  35-75 %                        Coarse-loamy     # BS >35 %

                Tas (Thap Salao series)                               Bar (Ban Rai series)                                     Lsk (Lan Suk series)








                Loamy-skeletal, mixed, superactive, isohyperthermic      Coarse-loamy, mixed, active, isohyperthermic          Coarse-loamy, mixed, semiactive, isohyperthermic
                Ultic  Haplustalfs                                    Ultic Haplustalfs                                        Typic Paleustalfs

                Parent material :  Alluvium from mainly granite              Relief : Gently undulating to Nearly flat  landform : Terrace, Alluvium fan
                # 10-7.5YR4-6/3-4                                                           l    Apg   12
                                     sl   Ap  30                      # 10-7.5YR4/1-3
                # mod. well drained                                                         cl   BAg   30
                (mottles within 100 cm.)                    spd       # 10-7.5YR5-6/1-2

                # mixed color subsoil   sl   Bt           Fine-loamy   # Somewhat poorly drained
                                             105                                            cl   Btg   105
                # argillic horizon                                    (mottles high chroma)
                                                                      # argillic horizon
                # BS >35 %
                                                          mod. well drained   # Endosaturation
                                    sgsl   Btc  200
                                                        Coarse-loamy   # lighter texture
                                                                                            sl   2Btg   200

                                                                      in subsoil (within 150 cm)
                Uti (Uthai series)                                    # BS >35 %



                Coarse-loamy, mixed, semiactive, isohyperthermic      Nch (Nong Chang series)


                Oxyaquic  Paleustalfs                                 Fine-loamy, mixed, semiactive, isohyperthermic

                                                                      Aeric  Endoaqualfs
                                                                                                                                                                115
   147   148   149   150   151   152   153   154   155   156   157