T Phn p, Thy s Sinh hc: 26 (2013): 43-49
43
BII THI
I HUYN M TNH LONG AN
Tr
1
1
n
1
1
1
B p c ng dngi hc C
Thông tin chung:
08/11/2012
20/06/2013
Title:
Improvement of soil fertility
and rice yield on old alluvial
soil at Moc Hoa district,
Long An province
Từ khóa:
Keywords:
Old alluvial soil, compost
amendment, rice-cash crop
alternation, soil nutrients
ABSTRACT
In the Mekong delta, old alluvial soil types are poor in soil nutrients.
Famers have applied only inorganic fertilizers for double rice cultivation
and have not paid much attention on using organic manure. With high
dose of inorganic N and P applied, intensive rice cultivation has led to
soil degradation and low rice yield. Objectives of this study were to find
the way to improve soil fertility and rice yield of mono-rice system on old
alluvial soil in Moc Hoa district, Long An province. Treatments were
arranged in randomized complete block design with 1) Double rice crops
Rice alternated with sesame;4) Rice alternated with peanut; 5) Rice
alternated with soybean. Experiment was conducted for 8 years. Results
showed that the system of rice crop alternated with cash crop led to
increase significantly soil available nitrogen, labile carbon content and
nitrogen mineralization in comparison with traditional rice cropping
practice. Organic amendment result the increases of labile carbon and
available nitrogen in soil compared to the rice treatment without compost
addition. As consequence, the rice yield has been improved by either
compost amendment or alternative cropping of rice and upland crops.
h
sinh
T Phn p, Thy s Sinh hc: 26 (2013): 43-49
44
1 M U
Nhiu v
u qu
ng nhu c
th gii (Olk ., 2002). Hin ti,
th c chim hai
n ba v i ding 14
triu ha n c
n l o ca
u (Cassman , 1995; Mahieu
ctv. suy git
n nay trong nhi
n t t ra s nghi
ng v n vng ca h th
(Cassman , 1997; Olk , 1996).
Mt s hin
d
thuc bo v thc v
Vi vi c nu
ng bi
n vng ca
sn xu n ph
u
bi ci thin ph nhiu t, ci
thi su
chn la bi p v u kin
sn phm.
u kin ngc ca h
th c, s ym
a thc v hn ch kh
m t a
cht h
m (N) hu dng b kim gi i dng to
p cht hy
t
ruma, 1976; Dobermann
t hu
b u t
sinh hc t p cht h
y t ng
ng kh c do u v
ng cht h
th gim dn gim kh m
hu dng (Stevanson et alng thi
s vi sinh v
gim mt s vi sinh vt.
T sung gim, hiu qu kinh
t mang l
c thc hin nhm ci thi
n
xu theo
ng sn xun vng.
2 N CU
m
(Plinthosols ng 4,7 thuc
lot chua vng cht hu
i cation
(CEC) th m tng s
i rt thp. Dung trng
tng m
ng b ng Fe
2
O
3
t
Al
3+
t cao (Bng 1). Nhng
ng bi i
thi t
ng.
Bng 1: Mt s ch c cm
Ch
pH
H2O
4,7
CEC (meq/100g)
3,75
Cht h
2,18
N
tng s
(%)
0,154
K
+
(meq/100g)
0,08
Ca
2+
(meq/100g)
0,48
Mg
2+
(meq/100g)
0,60
Na
+
(meq/100g)
0,06
Dung trng (g/m
3
)
1,32
xp (%)
43
Fe
2
O
3
(%)
2,84
Al
3+
(meq/100g)
2,53
Thnghim ng ruc thc hin di
hn t ti x Bnh
Tn, huyn Mc Ha, tnh Long An, theo th
thc khi hon ton ngu nhin gm nm
nghim thc vbn ln lp li vi
di
m
2
cho m m, gm
cc m hnh
nhsau:
Nghim th
Nghim th
tn/ha
T Phn p, Thy s Sinh hc: 26 (2013): 43-49
45
Nghim th
Nghim th u
ph
Nghim th u
c him, m t
c ly theo nghim th i v
i nhiu v
t - u,
mang v
n m m
hu dng, cht h t, carbon d
. Kh m
t
c thu thi v
Cht h
nh b Walkley-
Black. Cacbon d
bm ammonium
(N-NH
4
+
m nitrate (N-NO
3
-
ng
m mt nh bng
S li c x ng
ng
m thc m
3 KT QU O LUN
3.1 m (N) hu dt
Kt qu
cho thm hu dt m
thc l ng t 21,2 -
th i nghim th
t). m th
t hiu
u ki
tri
ng N hu dng
ng thi, nghim th
m
hu d t
qu c gi
hm hu dng t s
hp cht het
al., 1999).
m hu dt gi
nghim thm
3.2 Kh m (N)
3.2.1 Hng N-NH
4
+
Kh -NH
4
+
u
kin c thu
y thu
ng N-NH
4
+
c m th
-m thc
t qu c gi
tim h
-NH
4
+
u din ra m
nghim th -
nghim th n
ng N-NH
4
+
n hai nghim thc
m th
m thc
- ng N-NH
4
+
ng gim. Sau tu
ng N-NH
4
+
git
m th
-u
i nghim th t qu
ng cht hm
u
ki ng l
chuytrate.
T Phn p, Thy s Sinh hc: 26 (2013): 43-49
46
N-NH
4
+
3.2.2 ng N-NO
3
-
ng N-NO
3
-
c th
tr n
ho ng ca vi sinh v u kin
ng ln N-NH
4
+
-NO
3
-
ng N-NO
3
-
m
th - u phng so v
nghim th
u ki
y s n ca c ng vi sinh vt
-
NO
3
-
3.3 ng cht ht
Kt qu ng cht
h t bi ng t 2,14-2,8%
ng cht hp
u m nghim th
ng cht h
mt th i
m th t qu
nghim th
mi v thu hoc r i trong
ng cht ht
m th
ng oxy
t hu
m th
h ng cht h
c gi
h p chng
nm Trichoderma t. Chng n
din ra ti nghim th
0
10
20
30
40
50
60
0 tuần 2 tuần 4 tuần 8 tuần
Thời gian ủ
N-NH4+ (mg/kg đất)
Lúa - Lúa
Lúa+10 tấn HC - Lúa
Lúa - Mè
Lúa - Đậu Phộng
Lúa - Đậu Nành
0
5
10
15
20
25
0 tuần 2 tuần 4 tuần 8 tuần
Thời gian ủ
N-NO3- (mg/kg đất)
Lúa - Lúa
Lúa+10 tấn HC - Lúa
Lúa - Mè
Lúa - Đậu Phộng
Lúa - Đậu Nành
T Phn p, Thy s Sinh hc: 26 (2013): 43-49
47
3.4 Cacbon d y
Kt qu ng cacbon d
y mc
m th ng
cht hm thc
m th
ng cacbon d ca
nghim thi th
thm thi. Kt
qu c gi
c g trng
, thiu oxy, hong ca vi sinh vt
m kh
tha thc vt. Mt ngc
c, cht hn din ng hp
ch
ng cacbon d
hu trong h th
h
so vi nghim th
th c gi
m n cacbon d
h
ng h vi sinh vu kin
t vi sinh vt ho
ng cacbon d y.
T Phn p, Thy s Sinh hc: 26 (2013): 43-49
48
3.5
Kt qu m cho th t
m th
i nghim
th
y cht ht thun
l
vt hong cacbon
d
m hu d
sut ca h th
so vt qu p
vu ca Dobermann (2000),
tr t cao
i tr
t nghim th
bi i nghim thc
ng cht h u
qu s d m hu d
hong ca vi sinh vt.
4 KT LUN
Kh m hu dng, s
ng cacbon d
ht m th
m th
i
nghim th
h
U THAM KHO
1. Borthakur H. P. and N. N. Mazunda, 1968.
Effect of lime on nitrogen availability in paddy
soils, J. Indian Soil Sci. Soc, 16:143-147.
2. Casaman, K.R, A. Dorbermann, P.C. Stacruz,
G.C Gines, M.I. Samson, J.P.Descandota, J.M
Alcatara, M.A Dizon and D.C Oid, 1995. Soil
organic matter and the indigennous nitrogen
supply of intensived rice system in the tropics.
Plant and soil.
3. Cassman K. G., G. C. Gines, M. A. Dizon, M.
I. Samson and J. M. Alcantara, 1997. Nitrogen
use efficiency in tropical lowland rice systems:
Contributions from indigenous and applied
nitrogen, Field Crops Res. 47, 1-12.
4. Dobermann A. and C. Witt, 2000. The
potential impact of crop intensification on
carbon and nitrogen cycling in intensive rice
systems. In: Kirk, G.J.D., D.C. Olk, (Eds),
Carbon and nitrogen dynamics in Flooded
Soils. International Rice Research Institude,
Philippines, pp.1-25.
5. Mahieu N., D. C. Olk and E.W. Randall, 2002.
Multinuclear magnetic resonance analysis of
two humic acid fractions from lowland rice
soils, J. Environ. Qual. 31 : 421-430.
6. Nyle, C. Brady, Ray, and R. Weil, 1999.
Properties and Management of Soils in the
Tropics. Prentice Hall.
T Phn p, Thy s Sinh hc: 26 (2013): 43-49
49
7. Olk D. C. and K. G. Cassman, 2002. The role
of organic matter quality in nitrogen cycling
and yield trends in intensively cropped paddy
soils. p. 13551 to13558. In Proc. 17th World
Congress of Soil Science. 1421 Aug. 2002,
Bangkok, Thailand, International Union of
Soil Sciences.
8. Olk D. C., K. G. Cassman, E. W. Randall, P.
Kinchesh, L. J. Sanger and J. M. Anderson,
1996. Changes in chemical properties of
organic matter with intensified rice cropping in
tropical lowland soil, European Journal of Soil
Science, 47, 293-303.
9. Olk D. C., K. G. Cassman, N. Mahieu and
E.W.
Randall, 2002. Conserved chemical properties
of young humic acid fractions in tropical
lowland soil under intensive irrigated rice
cropping, European Journal of Soil Science,
49, 337349.
10. Ponnamperuma F. N., 1976. Specific soil
chemical characteristics for rice production in
Asia, IRRI Res. Paper Ser. 2:18.
11. Stevenson, F.J., 1986. Cycles of soil. John
Wiley and Sons, Inc. 1984-1996.
12.
ng cht cng
bu Long. Hi Khoa ht Vit
Nam. Tt 15, trang 26-32.