4 RESULTS AND DISCUSSION
Y3 (Pseudomonas putida) only affect
dehydrogenase and sediment carbon and nitrogen
content. There are some studies have confirmed that
the biological enrichment of inorganic nitrogen
fertilizers by farmland microorganisms reduces the
loss of nitrogen fertilizers (Shen et al., 1994). In
controlling nutrient supply, sediment microbial
biomass not only acts as a biocatalyst for many basic
reactions, but also equivalent to the fast turnover
library of sediment N and P elements (Burger and
Jackson, 2003). It can be seen that the microbial
activity and sediment physicochemical properties
mutually restrict and promote each other: On the one
hand, the metabolism of microorganisms improves
the physicochemical properties of the sediment; on
the other hand, the increase of the available organic
carbon and nitrogen content of sediment greatly
stimulates the activity of sediment microorganisms,
making better promote the sediment
physicochemical properties.
The suitable pH is favorable to the existence and
distribution of sediment salts. From the experimental
results, it can be known that the sediment pH was
basically neutral
Dehydrogenase is one of the main enzymes in
sediment, and its activity can be regarded as an
important indicator of sediment microbial activity
and functional diversity (Qin et al., 2005). Some
studies have shown that there are certain differences
in dehydrogenase activities in different sediments in
different environments, and different agrochemical
substances or pollutants may also affect the activity
of sediment dehydrogenase (Guo et al., 2000).
Chemical substances may also affect the microbial
diversity of sediment. At present, the influence of
organic compounds such as PAHs, organic
pesticides and microbial diversity of crude oil
sediment have been extensively studied at home and
abroad (Kalayama et al., 2001; Aisllabie et al., 2004).
The results showed that dehydrogenase reacts to
intracellular enzymes in the sediment,
microorganisms have an effect on the content of
sediment dehydrogenase. The addition of Y3
(Pseudomonas putida) can significantly increase
sediment dehydrogenase activity and accelerate
sediment self-repair.
Sediment organic carbon content is one of the
important indicators to measure sediment fertility.
The carbon source is an essential nutrient for the
growth of microorganisms. Organic carbon can be
easily absorbed by microorganisms and utilized. The
content of organic carbon in high-contamination
samples is slightly higher, some of the crude oil
contamination in sediment may be detected.It is also
possible that as pollution concentration goes on, the
Y3 (Pseudomonas putida) is seriously affected, the
utilization of organic carbon in the sediment is
getting lower and lower, so the content of the
retained organic carbon is slightly higher. The
organic carbon content in sediment with time first
increased and then decreased may be due to the
individual components of the crude oil in the
sediment can be used as nutrients for the
microorganisms, so the organic carbon content in
the sediment first increased.
The total sediment nitrogen content is the sum of
various forms of nitrogen in the sediment, including
organic nitrogen and inorganic nitrogen, but does
not include molecular nitrogen in the air. Sediment
total nitrogen content is related to the amounts of
microorganisms and dehydrogenase in the sediment
environment. Dongyun M et al showed that the
activity of soil dehydrogenase was significantly
positively correlated with the nitrogen application. A
timely and appropriate application of nitrogen could
promote the development of the root systems,
thereby increasing the amount of soybean roots,
increasing the secretion of roots.The powerful root
systems promotes the reproduction of sediment
microorganisms (Ma et al., 2007).
From the comparison of the N and P assay
results of each experimental group with the control
group. The content of N changed little, while the
content of P fluctuated with the concentration of
crude oil, the concentration of P and Y3
(Pseudomonas putida) in 8000mg/kg and
12000mg/kg experimental group were higher. It
shows that N and P are the main nutrient elements
and are related to the amounts of bacteria.
Congsheng Z et al pointed out that studying the
distribution characteristics of main nutrient elements
in soil is the important foundation for the study of
Geochemistry in wetland ecosystem,which is helpful
to the study of the plant rhizosphere ecosystem
(Zeng et al., 2009). Hanfeng X et al have confirmed
that there is a significant correlation between
organic carbon and N content in soil layers,
indicating that organic carbon and N have similar
spatial distribution rules; soil organic carbon and P
are related because P has small mobility and is
mainly influenced by organic matter and parent
material are similar to that of organic matter (Xiong